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    Abstract

    Water is one of the basic resources needed to sustain plant and animal life and

    ultimately human existence. Judicious use of this resource should be the concern of all

    people. This booklet gives a brief amount of estimated water resources and its efficient

    use. This booklet describes the hydrologic cycle, types, utilization and economic use of

    water. This will enable the farmer to use the water more scientifically and economically.

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    Introduction

    Water is an essential requirement of all living beings and indispensable for many

    human related activities. In nature it transports eroded material from mountains and

    forests to the plains and the sea. Man uses water to carry away his wastes, generate

    electric power, for navigation, industrial purposes and also as a source of recreation.

    Apart from all these, the role of water in agriculture is very significant Water is a limited

    resource and its efficient use is crucial to the survival of the human beings. Therefore,

    every effort must be made to make the best use of water so as to make possible a high

    level of continuous production. Several factors are to be kept in mind for the conservation

    and development of water resources. These are as follows:

    1. availability and source of water;

    2. climatic condition;

    3. quality of water;

    4. factors affecting water resources;

    5. distribution and variation of rainfall & water resources;

    6. competing demands; and

    7. nature of the soil. .

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    Water resources of a country constitute one of its vital assets. India receives annual

    precipitation of about 4000 km3. The rainfall in India shows very high spatial and

    temporal variability and paradox of the situation is that Mousinram near Cherrapunji,

    which receives the highest rainfall in the world, also suffers from a shortage of water

    during the non-rainy season, almost every year. The total average annual flow per year for

    the Indian rivers is estimated as 1953 km3. The total annual replenish able groundwater

    resources are assessed as 432 km3. The annual utilizable surface water and groundwater

    resources of India are estimated as 690 km3 and 396 km3 per year, respectively. With

    rapid growing population and improving living standards the pressure on our water

    resources is increasing and per capita availability of water resources is reducing day by

    day. Due to spatial and temporal variability in precipitation the country faces the problem

    of flood and drought syndrome. Overexploitation of groundwater is leading to reduction

    of low flows in the rivers, declining of the groundwater resources, and salt water intrusion

    in aquifers of the coastal areas. Over canal-irrigation in some of the command areas has

    resulted in water logging and salinity. The quality of surface and groundwater resources is

    also deteriorating because of increasing pollutant loads from

    Point and non-point sources. The climate change is expected to affect precipitation and

    water availability. So far, the data collection, processing, storage and dissemination

    have not received adequate attention. The efforts initiated under the Hydrology Project

    Phase-I and the development of the Decision Support System proposed under Hydrology

    Project Phase-II are expected to bridge some of the gaps between the developed advanced

    technologies of water resources planning, designing and management and their field

    applications. The paper presents availability and demands of water resources in India as

    well as describes the various issues and strategies for developing a holistic approach for

    sustainable development and management of the water resources of the country. It also

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    highlights integration of the blue and green flows and concepts of virtual water transfer

    for sustainable management of the water resources for meeting the demands of the

    present, without compromising the needs of future generations.

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    The overall navigable span of the inland watercourses in India is 14,500 km. The legal

    authority in control of the watercourses in the country is the Inland Waterways Authority

    of India or IWAI.

    The national watercourses in India can be divided into three and they are as follows:

    The Brahmaputra river system - extending from Sadiya to Dhubri

    The Ganga Bhagirathi Hooghly river - extending from Allahabad in Uttar Pradesh to

    Haldia in West Bengal

    The West Coast Canal from Kottapuram to Kollam together with Udyogmandal canal and

    Champakara canal.

    The water bodies are top tourist draws as well. Visitors from different corners of the

    world come to see these water resources. As a result, the travel and tourism sector of

    India is getting a boost. In addition, a large number of hotels and accommodations have

    come up around these visitor attractions to fulfill the requirements of the travelers. The

    country houses 13 major ports and approximately 180 small and medium harbors. The

    harbors manage over 95% of the commerce in the country and they also function as the

    principal entranceways for doing business. The important ports in India are as follows:

    Haldia, Kolkata, Visakhapatanam, Paradip, Chennai, Ennore, Cochin, Tuticorin,

    Mormugao, New Mangalore, Mumbai, Jawaharlal Nehru Port Trust, and Kandla.

    Rivers in India

    The country houses 12 rivers that are categorized as important rivers. The overall

    drainage basin watered by these rivers is more than 976,000 sq miles or 2,528,000 km2.

    All the important rivers in the country have their sources in any of the following areas:

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    Vindhya and Satpura mountain range, forming a part of the heart of the country

    The Karakoram and Himalayan mountain ranges

    Sahyadri or Western Ghats mountain range, forming a part of western India

    The biggest drainage basin in the country is created by the Ganges-Brahmaputra-

    Meghana river network and it covers a total area of approximately 620,000 sq miles or

    1,600,000 km2. The drainage basin of the Ganges river singularly covers a total area of

    around 420,000 sq miles or 1,100,000 km2.

    The source of the Ganges river is the Gangotri Glacier, which lies in the state of

    Uttarakhand. Subsequently, the river runs in the southeast direction, before pouring into

    the Bay of Bengal. The headwaters of the Gomti and Yamuna rivers lie in the western

    part of the Himalayan mountain range. These two rivers meet the Ganga in the flat

    terrain.

    The Brahmaputra River has its headwaters in the territory of Tibet. In the province of

    Tibet, people call it "Tsangpo" or Yarlung Tsangpo River. The river then penetrates the

    Indian Territory via the state of Arunachal Pradesh in the Northeast. Subsequently, the

    river moves to the west into Assam. In Bangladesh, the river meets the holy Ganga and

    the name of the river changes to the Jamuna River.

    A major branch of the river Ganga (Yamuna) is the Chambal River. The river has its

    headwaters in the Satpura and Vindhya mountain ranges. It runs to the east. From the

    same source, other rivers that have originated include the Tapti and Narmada and both of

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    these rivers pour into the Arabian Sea in the west. The river system that runs from the east

    to west forms 10% of the overall outpouring of water in India.

    All the rivers of the Deccan plateau have their headwaters in the Western Ghats mountain

    range. These rivers include the Godavari River, the Mahanadi River (passing across the

    delta formed by itself), Kaveri River, and Krishna River. All these rivers ultimately pour

    into the Bay of Bengal. Approximately 20% of the overall outpouring of the country is

    represented by these rivers.

    The intense precipitation in the rainy season in the southwest results in the swelling of the

    banks of the Brahmaputra and other rivers in India. This frequently leads to inundating of

    the bordering regions. Despite the fact that these rivers work as a fundamentally reliable

    source of fertilization and natural supply for the paddy cultivators, these inundations have

    resulted in loss of lives of a large number of people and force the population of the area to

    move to other places.

    Capes in India

    The major capes in India are as follows - Indira Point, the southernmost tip in India which

    is situated on the Great Nicobar Island, the Kanyakumari, the southern point of territory

    of India., Point Calimere, and Adam's (Rama's) Bridge.

    Gulfs in India

    The important gulfs in India are the Gulf of Kutch, the Gulf of Cambay, and the Gulf of

    Mannar. The country houses straits like the Ten Degree Canal, which dissevers the

    Andamans from the Nicobar Islands, the Palk Strait, which splits India from Sri Lanka,

    and the Eight Degree Canal, dissevering the Lakshadweep and Amindivi Islands from the

    Minicoy Island in the south.

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    The Indian Ocean and the Bay of Bengal are situated towards the south and east of the

    country and the Arabian Sea is located in the west. The Andaman Sea and the

    Lakshadweep Sea are smaller water bodies. The country houses four coral reefs and they

    lie in the Gulf of Mannar, the Andaman and Nicobar Islands, the Gulf of Kutch, and the

    Lakshadweep Islands.

    Lakes in India

    The major lakes in India are as follows - Vembanad Lake (Kerala), Sambhar Lake, (the

    biggest saltwater lagoon of the nation in Rajasthan), Loktak Lake (Manipur), Kolleru

    Lake (Andhra Pradesh), Chilka Lake (Orissa), Dal Lake (Kashmir), and Sasthamkotta

    Lake (Kerala).

    Water bodies that border India

    Given below are the names of the water bodies that surround India from different sides:

    Lakshadweep Sea in the southwest

    Arabian Sea in the west

    Bay of Bengal in the east

    Indian Ocean in the south

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    Problem Statement, hypothesis and rationale

    Total water in the world is estimated to be 1.5 billion cu km. About 95% of this is the

    salty water found in the oceans. This comes to around 1.425 billion cu km. Remaining 5%

    is fresh water i.e. only 75 million cu km. Out of this 75 million cu km 60 million cu km

    are immobilized as continuously frozen polar ice and snow, leaving only 15 million cu

    km as fresh liquid water for human, animal and plant needs. The world reserve of water

    resources is given in Fig. 1.

    World Water Resources

    Of the 15 million cu km of fresh water about 1 % (150,000 cu kin) is surface

    water found in rivers, lakes and streams and 99% is stored underground at varying depths.

    About half of this ground water (7,000,000 cu km) is stored at depths greater than 1000

    metres and is considered too expensive to pump to the surface for most uses. So total

    usable water in the world is 7 million cu km of fresh ground water at reasonable depth

    plus the 1,50,000 cu km of surface water.

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    III. Hydrologic Cycle

    Consumable water is obtained through precipitation. Precipitation occurs by the

    unending moisture cycle of the earth called hydrologic cycle. Moisture is constantly

    circulating between the land, the ocean and the atmosphere. This hydrologic cycle has

    neither a beginning nor an end. Radiation from the sun evaporates water from ocean,

    lakes, rivers into the atmosphere. Transpiration also takes place from the vegetation and

    adds water to the atmosphere. The water vapour rises and collects to form clouds. Under

    certain conditions, the cloud moisture condenses and falls back to the earth as rain, hail,

    sleet or snow. The whole process is diagrammatically given in two Figures 2a & 2b. The

    Hydrologic Cycle.

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    Hydrologic cycle.

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    Hydrologic cycle.

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    Types of water resources

    OF all the planets renewable resources, water has a unique place. It is essential for sustaining all

    forms of life, food production, economic development, and for general well-being. It is

    impossible to substitute for most of its uses, difficult to de-pollute, expensive to transport, and it is

    truly a unique gift to mankind from nature. Water is also one of the most manageable of the

    natural resources as it is capable of diversion, transport, storage, and recycling. All these

    properties impart to water its great utility for human beings. The surface water and groundwater

    resources of the country play a major role in agriculture, hydropower generation, livestock

    production, industrial activities, forestry, fisheries, navigation, recreational activities, etc.

    According to National Water Policy in the planning and operation of systems, water allocation

    priorities should be broadly as: (i) drinking water, (ii) irrigation, (iii) hydropower, (iv) ecology,

    (v) agro-industries and non-agricultural industries, and (vi) navigation. India receives annual

    precipitation of about 4000 km3, including snowfall. Out of this, monsoon rainfall is of the order

    of 3000 km3. Rainfall in India is dependent on the south-west and north-east monsoons, on

    shallow cyclonic depressions and disturbances and on local storms. Most

    of it takes place under the influence of south-west monsoon between June and September except

    in Tamil Nadu, where it is under the influence of north-east monsoon

    during October and November. India is gifted with a river system comprising more than 20 major

    rivers with several tributaries. Many of these rivers are perennial and some

    of these are seasonal. The rivers like Ganges, Brahmaputra and Indus originate from the

    Himalayas and carry water throughout the year. The snow and ice melt of the Himalayas

    and the base flow contribute the flows during the lean season. Lal2 mentioned that more than 50%

    of water resources of India are located in various tributaries of these river systems. Average water

    yield per unit area of the Himalayan rivers is almost double that of the south peninsular rivers

    system, indicating the importance of snow and glacier melt contribution from the high mountains.

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    Apart from the water available in the various rivers of the country, the groundwater is also an

    important source of water for drinking, irrigation, industrial uses, etc. It accounts

    for about 80% of domestic water requirement and more than 45% of the total irrigation in the

    country. As per the international norms, if per-capita water availability is less than 1700 m3 per

    year then the country is categorized as water stressed and if it is less than 1000 m3 per capita per

    year then the country is classified as water scarce. In India per

    Capita surface water availability in the years 1991 and 2001 were 2309 and 1902 m3 and these

    are projected to reduce to 1401 and 1191 m3 by the years 2025 and 2050 respectively. Hence,

    there is a need for proper planning, development and management of the greatest assets of the

    country, viz. water and land resources for raising the standards of living of the millions of people,

    particularly in the rural areas.

    Mans influence on hydrological cycle

    The hydrological cycle is being modified quantitatively and qualitatively in most of the

    river basins of our country as a result of the developmental activities such as construction

    of dams and reservoirs, land use change, irrigation, etc.Such human activities affecting

    the hydrological regime can be classified into four major groups: (i) activities which

    affect river runoff by diverting water from rivers, lakes, and reservoirs or by groundwater

    extraction, (ii) activities modifying the river channels, e.g. construction of reservoirs and

    ponds, levees and river training, channel dredging, etc.(iii) activities due to which runoff

    and other water balance components are modified due to impacts of basin surface e.g.

    agricultural practices, drainage of swamps, forestation or deforestation, urbanization, etc.

    and (iv) activities which may induce climate changes at regional or global scale,e.g.

    modifying the composition of atmosphere by increasing the greenhouse gases or by

    increased evaporation caused by large scale water projects. For understanding the effects

    appropriately, hydrological modeling approaches have to be adopted3 .

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    Monsoon and its forecasting

    The word monsoon is derived from mausim, Arabic word, which means season and the

    word is applied to winds whose direction is reversed completely from one season to the

    next season. The largest precipitation accumulations for periods greater than 24 h are

    associated with the Asian monsoon. Normal duration of monsoon in India is about 100 to

    120 days beginning from first June. In India, the two monsoon seasons (the southwest

    monsoon in June to September and the northeast monsoon in November December)

    bring forth rains. An important feature affecting the rainfall in India is the change in the

    direction of wind currents that occurs in different months. In May when the weather is

    very hot, the south-east trade winds from the south Indian Ocean cross the equator and

    after deflecting, due to rotation of the earth, extend rapidly into the north Indian Ocean,

    viz. the Bay of Bengal in early May and afterwards get established over both the sea

    areas. This westerly current, which extends from the Arabic coast to the China Sea across

    India, is known as the southwest monsoon. In winter season, the wind currents over India

    Blow from north to south.

    Precipitation variability

    The long-term average annual rainfall for the country is 1160 mm, which is the highest

    anywhere in the world for a country of comparable size2. The annual rainfall in India

    however fluctuates widely. The highest rainfall in India of about 11,690 mm is recorded

    at Mousinram near Cherrapunji in Meghalaya in the northeast5. In this region rainfall as

    much as 1040 mm is recorded in a day. At the other extreme are places like Jaisalmer, in

    the west, which receives barely 150 mm of rain. Though the average rainfall is adequate,

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    nearly three-quarters of the rain pours down in less than 120 days, from June to

    September. As much as 21% of the area of the country receives less than 750 mm of rain

    annually while 15% receives rainfall in excess of 1500 mm. Precipitation generally

    exceeds 1000 mm in areas to the east of Longitude 78E. It reaches nearly to 2500 mm

    along almost the entire west coast and over most of Assam and sub-Himalayan

    West Bengal. Large areas of peninsular India receive rainfall less than 600 mm. Annual

    rainfall of less than 500 mm is experienced in western Rajasthan and adjoining parts of

    Gujarat, Haryana and Punjab. Rainfall is equally low in the interior of the Deccan lateau,

    east of the Sahyadris. A third area of low precipitation is around Leh in Kashmir.

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    Figure 1. Distribution of normal annual rainfall in India (IMD, 2004).

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    Water resources of India

    Although India occupies only 3.29 million km2 geographical areas, which forms 2.4% of

    the worlds land area, it supports over 15% of the worlds population. The population of

    India as on 1 March 2001 stood at 1,027,015,247 persons. Thus, India supports about

    1/6th of world population, 1/50th of worlds land and 1/25th of worlds water resources7.

    India also has a livestock population of 500 million, which is about 20% of the worlds

    total livestock population. More than half of these are cattle, forming the backbone of

    Indian agriculture. The total utilizable water resources of the country are assessed as 1086

    km3. A brief description of surface and groundwater water resources of India is given

    Below.

    Surface water resources

    In the past, several organizations and individuals have estimated water availability for the

    nation. Recently, the National Commission for Integrated Water Resources

    Development8 estimated the basin-wise average annual flow in Indian river systems as

    1953 km3. The details are given in Table 1. Utilizable water resource is the quantum of

    withdraw able water from its place of natural occurrence. Within the limitations of

    physiographic conditions and socio-political environment, legal and constitutional

    constraints and the technology of development available at present, utilizable quantity of

    water from the surface flow has been assessed by various authorities differently. The

    utilizable annual surface water of the country is 690 km3 (Table 1)9. There is

    considerable scope for increasing the utilization of water in the GangaBrahmaputra

    basins by construction of storages at suitable locations in neighboring countries.

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    Table 1. Basin wise average flow and utilizable water9 (in km3/year)

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    Groundwater resources

    The annual potential natural groundwater recharge from0 rainfall in India is about 342.43

    km3, which is 8.56% of total annual rainfall of the country. The annual potential

    groundwater recharge augmentation from canal irrigation system is about 89.46 km3.

    thus, total replenish able groundwater resource of the country is assessed as 431.89%.

    After allotting 15% of this quantity for drinking, and 6 km3 for industrial purposes, the

    remaining can be utilized for irrigation purposes. Thus, the available groundwater

    resource for irrigation is 361 km3, of which utilizable quantity (90%) is 325 km3. The

    estimates by the Central Groundwater Board (CGWB) of total replenish able groundwater

    resource, provision for domestic, industrial and irrigation uses and utilizable groundwater

    resources for future use are given in Table 2. The basin wise per capita ater

    Availability varies between 13,393 m3 per annum for the BrahmaputraBarak basin to

    about 300 m3 per annum for the Sabarmati basin. The state-wise estimates of dynamic

    Groundwater (fresh) resource made by the CGWB10 is given in Table 3. The basin-wise

    groundwater potential of the country is given in Table 4.

    Water requirements of India.

    Traditionally, India has been an agriculture-based economy. Hence, development of

    irrigation to increase agricultural Production for making the country self-sustained and for

    poverty alleviation has been of crucial importance for the planners. Accordingly, the

    irrigation sector was assigned a very high priority in the 5-year plans. Giant schemes like

    the Bhakra Nangal, Hirakud, Damodar Valley, Nagarjunasagar,Rajasthan Canal project,

    etc. were taken up to increase irrigation potential and maximize agricultural production.

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    Long-term planning has to account for the growth of population. According to National

    Water Policy1, the production of food grains has increased from around 50 million tones

    in the fifties to about 203 million tones in the year 19992000. A number of individuals

    and agencies have estimated the likely population of India by the year 2025 and 2050.

    According to the estimates adopted by NCIWRD9, by the year 2025, the population is

    expected to be 1333

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    million in high-growth scenario and 1286 million in low growth scenario. For the year

    2050, high rate of population growth is likely to result in about 1581 million people

    While the low growth projections place the number at nearly 1346 million. Keeping in

    view the level of consumption, losses in storage and transport, seed requirement, and

    buffer stock, the projected food-grain and feed demand for 2025 would be 320 million

    tones (high-demand scenario) and 308 million tones (low-demand scenario). The

    requirement of food grains for the year 2050 would be 494 million tones (high-demand

    scenario) and 420 million tones (low demand scenario). Table 5 provides details of the

    population of India and per capita water availability as well as utilizable surface water for

    some of the years from 1951 to 2050 (projected). The availability of water in India shows

    wide spatial and temporal variations. Also, there are very large inter annual variations.

    Hence, the general situation of availability of per capita availability is much more

    alarming than what is depicted by the average figures.

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    Domestic use

    Community water supply is the most important requirement and it is about 5% of the total

    water use. About 7 km3 of surface water and 18 km3 of groundwater are being used

    for community water supply in urban and rural areas. Along with the increase in

    population, another important change from the point of view of water supply is higher

    rate of urbanization. According to the projections, the higher is the economic growth, the

    higher would be urbanization. It is expected that nearly 61% of the population will be

    living in urban areas by the year 2050 in high-growth scenario as against 48% in low

    growth scenario. Different organizations and individuals have given different norms for

    water supply in cities and rural areas. The figure adopted by the NCIWRD9 was 220 liter

    per capita per day (lpcd) for class I cities. For the cities other than class I, the norms are

    165 for the year 2025 and 220 lpcd for the year 2050. For rural areas, 70 lpcd and 150

    lpcd have been recommended for the years 2025 and 2050. Based on these norms and

    projection of population, it is estimated that by 2050, water requirements per year for

    domestic use will be 90 km3 for low demand scenario and 111 km3 for high demand

    scenario. It is expected that about 70% of urban water requirement and 30% of rural water

    requirement will be met by surface water sources and the remaining from groundwater.

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    Irrigation

    The irrigated area in the country was only 22.6 million hectare (Mha) in 195051. Since

    the food production was much below the requirement of the country, due attention was

    paid for expansion of irrigation. The ultimate irrigation potential of India has been

    estimated as 140 Mha. Out of this, 76 Mha would come from surface water and 64 Mha

    from groundwater sources. The quantum of water used for irrigation by the last century

    was of the order of 300 km3 of surface water and 128 km3 of groundwater, total 428

    km3. The estimates indicate that by the year 2025, the water requirement for irrigation

    would be 561 km3 for low-demand scenario and 611 km3 for high-demand scenario.

    These requirements are likely to further increase to 628 km3 for low-demand scenario

    and 807 km3 for high-demand scenario by 2050.

    Hydroelectric power

    The hydropower potential of India has been estimated at 84,044 MW at 60% load factor.

    At the time of independence, the installed capacity of hydropower projects was 508 MW.

    By the end of 1998, the installed hydropower capacity was about 22,000 MW. The status

    of hydropower development in major basins is highly uneven. According to an estimate,

    India has plans to develop 60,000 MW additional hydropower by the twelfth five-year

    plan. It includes 14,393 MW during the tenth five-year plan (20022007); 20,000 MW

    during eleventh (20072012) and 26,000 MW during the twelfth (20122017) five-year

    plans. A potential of the order of 10,000 MW is available for development of small

    hydropower projects in the Himalayan and sub-Himalayan regions of the country.

    Therefore, it is not only desirable but also a pressing need of time to draw a master plan

    for development of small, medium and large hydro-schemes for power generation.

    Industrial water requirement

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    Rough estimates indicate that the present water use in the industrial sector is of the order

    of 15 km3. The water use by thermal and nuclear power plants with installed capacities of

    40,000 MW and 1500 MW (1990 figures) respectively, is estimated to be about 19 km3.

    In view of shortage of water, the industries are expected to switch over to water efficient

    technologies. If the present rate of water use continues, the water requirement for

    industries in 2050 would be 103 km3; this is likely to be nearly 81 km3 if water saving

    technologies are adopted on a large scale.

    Total water requirements

    Total annual requirement of water for various sectors has been estimated and its break up

    is given Table 6. With the increasing population as well as all round development in the

    country, the utilization of water has also been increasing at a fast pace. In 1951, the actual

    utilization of surface water was about 20% and 10% in the case of groundwater. The

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    utilizable water in river basins is highly uneven. For example in the Brahmaputra basin,

    which contributes 629 billion m3 of surface water of the countrys total flow, only 24

    billion m3 is utilizable.

    Water resources management in India

    In view of the existing status of water resources and increasing demands of water for

    meeting the requirements of the rapidly growing population of the country as well as the

    problems that are likely to arise in future, a holistic, well planned long-term strategy is

    needed for sustainable water resources management in India. The water resources

    management practices may be based on increasing the water supply and managing the

    water demand under the stressed water availability conditions. Data monitoring,

    processing, storage, retrieval and dissemination constitute the very important aspects of

    the water resources management. These data may be utilized not only for management

    but also for the planning and design of the water resources structures. In addition to these,

    now days decision support systems are being developed for providing the necessary

    inputs to the decision makers for water resources management. Also, knowledge sharing,

    peoples participation, mass communication and capacity building are essential for

    effective water resources management. Some important aspects of such strategies are

    described as follows.

    Flood management

    Among all natural disasters, floods are the most frequent to be faced in India. Floods in

    the eastern part of India, viz.Orissa, West Bengal, Bihar and Andhra Pradesh in the recent

    past, are striking examples. According to the information published by different

    government agencies, the tangible and intangible losses due to floods in India are

    increasing at alarming rate. As reported by the Central Water Commission (CWC) under

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    the Ministry of Water Resources, Government of India, the annual average area affected

    by floods is 7.563 Mha.

    Drought management

    The drought-prone area assessed in the country is of the order of 51.12 Mha. The

    planning and management of the effects of drought appear to have a low priority due to

    associated randomness and uncertainty in defining the start and end of droughts. Further,

    most of the drought planning and management schemes are generally launched after

    persisting drought conditions. The traditional system of drought monitoring and

    estimating losses by crop cutting needs replacement with real time remote sensing, GIS,

    GPS and modeling techniques for ensuring transparency and quick response. Scope of

    losses may be extended to groundwater depletion, damage to perennial trees, plantations,

    orchards and depletion in fertility of livestock.

    Groundwater management

    To protect the aquifers from overexploitation, an effective groundwater management

    policy oriented towards promotion of efficiency, equity and sustainability is required.

    Agricultural holdings in India are highly fragmented and the rural population density is

    large. The exploitation of groundwater resources should be regulated so as not to exceed

    the recharging possibilities, as well as to ensure social equity. The detrimental

    environmental consequences of over-exploitation of groundwater need to be effectively

    prevented by the Central and State Governments. Overexploitation of groundwater should

    be avoided, especially near the coasts to prevent ingress of seawater into freshwater

    aquifers1. Clearly, a joint management approach combining government administration

    with active people participation is a promising solution.

    Conjunctive use of surface and groundwater

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    Large canal infrastructure network for providing irrigation has been the prime goal of the

    Government of India, since the first five-year plan, which continued up to seventh five-

    year plan. In some of the irrigation project commands such as Sarda Sahayak in UP,

    Gandak in Bihar, Chambal in Rajasthan, Nagarjuna Sagar in Andhra Pradesh,

    Ghataprabha and Malaprabha in Karnataka etc., problems of water logging are being

    faced. The main reason for excessive use of surface water as compared to groundwater is

    its much lower price for irrigation as compared to the cost incurred in using

    groundwater. Water logging problems could be overcome if conjunctive use of surface

    and groundwater is made. Groundwater utilization for irrigation in waterlogged areas can

    help to lower the groundwater table and reclaim the affected soil. Over exploitation of

    groundwater in areas like Mehsana, in Gujarat; parts of Meeurt and Varanasi districts in

    Uttar Pradesh, Coimbatore in Tamil Nadu and Karnal district in Haryana etc. have

    resulted in mining of groundwater20. Many research workers have focused the causes of

    waterlogging21. Several groundwater flow modeling studies have focused on assessing

    the waterlogged areas and measures to control problems of water logging and

    salinization22,23. It is desirable that the irrigation needs for fulfilling crop water

    requirements should be satisfied by judicious utilization of available canal water in

    conjunction with groundwater so as to keep the water table within the acceptable range.

    Thus, the optimal conjunctive use of the regions surface and groundwater resources

    would help in minimizing the problems of water logging and groundwater mining.

    Water conservation

    Water conservation implies improving the availability of water through augmentation by

    means of storage of water in surface reservoirs, tanks, and soil and groundwater zone. It

    emphasizes the need to modify the space and time availability of water to meet the

    demands. This concept also highlights the need for judicious use of water. There is a great

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    potential for better conservation and management of water resources in its various uses.

    On the demand side, a variety of economic, administrative and community-based

    measures can help conserve water. Also, it is necessary to control the growth of

    population since large population is putting massive stress on all natural resources. Since

    agriculture accounts for about 69% of all water withdrawn, the greatest potential for

    conservation lies in increasing irrigation efficiencies. Just a 10% improvement in

    irrigation efficiency could conserve enough water to double the amount available for

    drinking. In India, sprinkler irrigation is being adopted in Haryana, Rajasthan, Uttar

    Pradesh, Karnataka, Gujarat and Maharashtra. The use of sprinkler irrigation saves about

    56% of water for the winter crops of bajra and jowar, while for cotton, the saving is about

    30% as compared to the traditional gravity irrigation. An important supplement to

    conservation is to minimize the wastage of water. In urban water supply, for example,

    almost 30% of the water is wasted due to leakages, carelessness, etc. while most metro

    cities face deficit in supply of water. It is, therefore, imperative to prevent wastage. In

    industries also, there is a scope for economy in the use of water.

    Rainwater harvesting

    Rainwater harvesting is the process to capture and store rainfall for its efficient utilization

    and conservation to control its runoff, evaporation and seepage. Some of the benefits of

    rainwater harvesting are:

    It increases water availability

    It checks the declining water table

    It is environmentally friendly

    It improves the quality of groundwater through dilution,

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    Mainly of fluoride, nitrate, and salinity, and

    It prevents soil erosion and flooding, especially in the

    Urban areas.

    Even in ancient days, people were familiar with the methods of conservation of rainwater

    and had practiced them with success. Different methods of rainwater harvesting were

    developed to suit the geographical and meteorological conditions of the region in various

    parts of the country. Traditional rainwater harvesting, which is still prevalent in rural

    areas, is done by using surface storage bodies like lakes, ponds, irrigation tanks, temple

    tanks, etc. For example,Kul (diversion channels) irrigation system which carries water

    from glaciers to villages is practiced in the Spiti area of Himachal Pradesh. In the arid

    regions of Rajasthan, rainwater harvesting structures locally known as Kund (a covered

    underground tank), are constructed near the house or a village to tackle drinking water

    problem. In Meghalaya, Bamboo Rainwater Harvesting for tapping of stream and spring

    water through bamboo pipes to irrigate plantations is widely prevalent. The system is so

    perfected that about 1820 liters of water entering the bamboo pipe system per minute is

    transported over several hundred meters. There is a need to recharge aquifers and

    conserve rainwater through water harvesting structures. In urban areas, rainwater will

    have to be harvested using rooftops and open spaces. Harvesting rainwater not only

    reduces the possibility of flooding, but also decreases the communitys dependence on

    groundwater for domestic uses.

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    Recycle and reuse of water

    Another way through which we can improve freshwater Availability is by recycle and

    reuse of water. It is said that in the city of Frankfurt, Germany, every drop of water is

    recycled eight times. Use of water of lesser quality, such as reclaimed wastewater, for

    cooling and fire fighting is an attractive option for large and complex industries to reduce

    their water costs, increase production and decrease the consumption of energy. This

    conserves better quality waters for potable uses. Currently, recycling of water is not

    practiced on a large scale in India and there is considerable scope and incentive to use this

    alternative. Estimates25 show that recyclable water is between 103 and 177 km3/year for

    low and high population projections.

    People participation and capacity building for making the people of various sections of

    the society aware about the different issues of water resources man SPECIAL

    management, a participatory approach may be adopted. Mass communication

    programmers may be launched using the modern communication means for educating the

    people about water conservation and efficient utilization of water. Capacity building

    should be perceived as the process whereby a community equips itself to become an

    active and well-informed partner in decision making. The process of capacity building

    must be aimed at both increasing access to water resources and changing the power

    relationships between the stakeholders. Capacity building is not only limited to officials

    and technicians but must also include the general awareness of the local population

    regarding their responsibilities in sustainable management of the water resources. Policy

    decisions in any water resources project should be directed to improve knowledge,

    attitude and practices about the linkages between health and hygiene, provide higher

    water supply service levels and to improve environment through safe disposal of human

    waste. Sustainable management of water requires decentralized decisions by giving

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    authority, responsibility and financial support to communities to manage their natural

    resources and thereby protect the environment.

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    Work Plan

    On an average, India receives about 120 cm of precipitation in a year, mostly as

    rainfall. .On volume basis this is 394.5 million hectare metre (m. ham). (let us take 400 m.

    ha m as an approximate figure). The main source of precipitation is rainfall. India is a vast

    country in the world compared to any other country having an annual rainfall of about

    117 to 120 cm. Rainfall over the entire country during monsoon is nearly 75% of the

    mean annual, while during pre-monsoon and post -monsoon seasons the country receives

    almost the same amount of rainfall which is about 10 to 11 % of the mean annual. In

    January and February the country receives just about 3.5% of the mean annual rainfall

    and it is mostly confined to Jammu & Kashmir, Himachal Pradesh, Po.jab, North-West

    U.P., North Bengal and Assam. Different monsoons is shown below in Tables 1 & 2

    respectively.

    Table 1 .Rainfall distribution In various states of India (in mm)

    Sl.No. States Meteorological

    Sub-divisions

    Rainfall

    1 Andhra Pradesh Costal

    Telangana

    Rayalaseema

    935

    891

    893

    2 North Eastern States Arunachal Pradesh

    Assam

    Nagaland

    3736

    2423

    2065

    3 Bihar Plateau

    Plains

    1490

    1267

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    4 Gujarat Gujarat

    Saurastra

    1002

    590

    5 Haryana Haryana 772

    6 Himachal Pradesh Himachal Pradesh 1971

    7 Jammu & Kashmir Jammu & Kashmir 967

    8 Karnataka Costal

    North Interior

    South Interior

    3366

    837

    914

    9 Kerala Kerala 2961

    10 Madhya Pradesh West

    East

    1144

    1470

    11 Maharastra Madhya

    Marathwada

    Vidarbha

    Konkan

    706

    780

    1124

    2871

    12 Orissa Orissa 1486

    13 Punjab Punjab 760

    14 Rajasthan West

    East

    465

    937

    15 Tamil Nadu Tamil Nadu

    Pondichery

    1008

    1335

    16 Uttar Pradesh East

    Plains

    Hills

    873

    806

    1840

    17 West bengal Sub-Himalayan

    Gangetic

    3079

    1846

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    Note: The above mentioned figures are based on the total rainfall received from

    June to September during 1977-78.

    On the basis of these, different regions of the country can be divided into three

    categories viz., high rainfall areas, medium rainfall areas and low areas. The areas

    receiving above 1,150 mm annual rainfall are high rainfall areas, those receiving between

    750 and 1,150 mm are medium rainfall areas and the areas with annual rainfall below 750

    mm are low rainfall areas.

    Table 2 .Distribution and extent of rainfall through different monsoons

    Sl.No. Time & type of monsoon % of rainfall

    1. South West monsoon (June to Sept) 75

    2. Post monsoon season ((Oct to Dec.) 1011

    3. Winter season ( Jan to Feb) 3-4

    4. Pre-monsoon season ( Mar to May) 10-11

    .

    IV. Types of Water Resources Based on Uses

    According to the uses water resources may be classified into three main groups.

    1. For consumptive uses

    2. Partially consumptive uses

    3. Non consumptive uses

    1. Consumptive uses

    Irrigation, urban and rural water supplies are grouped in this ' category, since, in these

    situations, water is directly consumed by living beings.

    2. Partially consumptive uses

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    Use of water for domestic and industrial purposes, thermal and nuclear power

    generation, etc. are partially consumptive as, a part of the water can be renewed for reuse

    after proper conditioning.

    3. Non-consumptive uses

    This includes the quantity required for hydro-power generation, navigation,

    pollution control, recreation, preservation of fish and wild life etc.

    V. Water Resources in India

    According to the placement, water resources of India are : divisible into twodistinct categories:

    A. Surface water resources

    B. Ground water resources

    The precipitation that falls on land is the ultimate source for both the categories of

    water resources.

    A. Surface water resources

    When rain falls, a sizable portion is intercepted by the vegetation, or temporarilydetained in surface depressions. When the available interception or the depression

    storages are completely exhausted and when the rainfall intensity at the soil surface

    exceeds the infiltration capacity of the soils, the over land flow begins. This water reaches

    the rivers, streams, lakes, surface reservoirs, darns, etc. Our irrigation mainly depends on

    surface water resources. Runoff water from streams and rivers is stored in reservoirs or is

    diverted directly through canal system for irrigation. Water re- sources region can be

    planned on the basis of river basins.

    1. River systems in India

    Rivers are the main source of surface water. A river basin has well defined

    watershed boundary and also has relationship with ground water resources in most of the

    cases.

    India has been divided into six river basins for the purpose of assessment of the

    available water resources. The following table will present the location, climatological

    factors, annual run-off and approximate volume of water of these six river basins. These

    are:

    a. Indus basin

    b. Ganga system

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    c. Brahmaputra system

    d. East coast

    e. West coast and

    f. Rajputana region

    Table 3 -Different river basins of India

    Sl.

    No.

    Important

    River basin

    State in the

    region

    Cath

    Men

    t

    Area

    (m

    ha)

    Avge

    Annua

    l

    Precipi

    Tation

    M ha

    metre

    Total

    Precipi

    -

    Tation

    M ha

    metre

    Mean

    Tempe-

    Rature

    OC

    Avg

    Annua

    l

    Runoff

    M ha

    metre

    Volu

    me

    Of

    Wate

    r

    M ha

    metr

    e

    1 Ravi, Beas,

    Sutlej

    J &

    Kashmir,

    Punjab

    Haryana

    Himachal

    prade

    35.4

    0

    56.00 19.82 1260 07.94 04.93

    2 Ganga,

    Yamuna

    Chambal

    gogra

    Guwduk,

    Kosi

    U.P. Bihar,

    M.P

    Rajasthan

    & West

    Bengal

    97.6

    0

    111 108.3 16.80 48.96 18.50

    3 Brahmaputra

    ,

    Subausiri,

    Manar

    Teest

    Assam,

    Meghalaya

    ,

    Nagaland

    West

    Bengal

    50.6

    2

    122 61.72 08.20 38.08 1.23

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    4 Cavery,

    Krishna,

    Godavari,

    Mahanadi,

    Subarnarekha

    Damodal

    Madhya

    Prades

    Bihar,

    Orissa,

    West

    Bengal

    A.P.

    Maharastra

    Karnataka

    Tamil

    Nadu

    121 109 131.9 26.1 41.19 33.80

    5 Tapti,

    Narmada,

    Mahi,

    Sabarmati

    Gujarat,

    Kerala

    Maharastra

    Karnataka

    49.1

    6

    122 59.98 25.5 31.06 6.92

    6 Luni &Ghagaoa

    Rajasthan 16.80

    29.00 04.87 26.2 - 1.22

    7 Total 370.

    61

    --- 386.7 --- 167.2 66.6

    The assessment of this surface reservoir is also calculated by lots of assumptions

    on run-off, rainfall temperature etc. So this resource can be an approximate figure. All

    these water resources cannot be utilized due to the limitations imposed by the

    physiographic factors.

    Surface water stored in reservoirs or diverted directly is distributed for irrigation

    through the canal irrigation network. A canal starts either from a water storage dam or

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    diversion darn. Irrigation water flows through the complete canal system before it reaches

    the farmer's field to be irrigated. The canal network consist- of canals, distributaries,

    water courses and field channels.

    B. Ground Water Resources

    The main source of ground water is rainfall. However, ground water recharge is

    supplemented by other sources such as seepage from canals and field channels, ponds,

    tanks, effluent drainage from rivers, deep percolation from irrigated fields, etc. A part of

    any of these water sources that infiltrates into surface soil may continue to move laterally

    at a shallow depth. This water which flows below the soil surface may eventually reach

    the stream channel. This flow of water below the surface is called sub surface run off. A

    part of the sub surface run-off may enter the stream promptly, whereas the remaining part

    may percolate deeply into the soil and remain above the water table in the zone of

    saturated flow. This water table shows the upper level of ground water in the earth.

    The total run-off in the stream channel includes the melted snow, the surface run-

    off, the sub surface run-off and the ground water run -off. The portion of run-off water,

    after infiltration reaches the ground water table, together with the contribution made to

    ground water from a neighbouring basins, effluent rivers, natural lakes, ponds, artificial

    storage reservoirs, and canals irrigations r constitutes the ground water resources.

    This whole process is diagramatically explained below Figure 2

    1. Ground water regions or India

    The availability and development potential of ground water in India on the basis

    of geological consideration can be described under the following three broad categories:

    a. Unconsolidated rocks

    b. Semi-consolidated rocks

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    Methodology

    Utilization of Water Resources

    Water resources are utilized mainly for three purposes:

    1. Irrigation2. Industrial3. DomesticOut of these three, irrigation is the major consumer of water resources. The total

    utilization of water in India is depicted in the following flow-chart in Figure 3. on the

    Total Precipitation.

    Total Precipitation

    Our water resources are insufficient to meet the long term requirement of

    agriculture, industry and other uses, unless its judicious and economic uses are ensured.

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    The total geographical area of our country is 328.7 million hectares (m.ha). About

    42% of this area is under cultivation i.e., 140.7 m ha. Only 26.6% of this area is irrigated

    through various sources. Following tables give the area irrigated by different sources

    indifferent years and the States.

    Table 6 .Irrigation potential or different sources or water

    (Area in million hectars)

    Sl.No. Sources 1981-82 1982-83 1983-84 1984-

    85

    1 Government canals 14.68

    (36.3)

    14.87

    (37.2)

    15.74

    (37.5)

    15.33

    (36.5)

    2 Private canals 0.84

    (2.1)

    0.495

    (1.2)

    0.495

    (1.2)

    0.495

    (1.2)

    3 Tanks 3.506

    (8.8)

    3.112

    (7.8)

    3.783

    (9.0)

    3.330

    (8.0)

    4 Tubewe/ls 9.900

    (24.9)

    10:684

    (26.7)

    10.973

    (26.I)

    11.265

    (26.9)

    5 Other wells 8.267

    (20.8)

    8.428

    (21.1)

    8.548

    (20.4)

    8.723

    (20.9)

    6 Other sources 2.566

    (6.5)

    2.375

    (6.0)

    2.411

    (5.8)

    2.600

    (6.2)

    7 Total irrigated area 39.764 39.969 41.995 41.779

    (in bracket per cent of the area is shown)

    Irrigation is mainly carried out through minor irrigation schemes as well as major

    and medium irrigation schemes. Our nation has the potentiality to explore maximum

    amount of water but technology and attempts have to be developed for the utilization.

    Following table gives the potential created and utilized water.

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    Table 7. Net area irrigated by different sources (in thousand ha)

    Sl

    .No.

    States Canals Tanks Tube

    wells

    Other

    wells

    Other

    source

    Total

    Irrigat

    ed area

    1 Andhra Pradesh 1627 1100 114 470 126 3437

    2 Assam 362 --- --- --- 210 572

    3 Bihar 896 118 846 225 475 2760

    4 Gujarat 245 25 130 999 15 1414

    5 Haryana 1036 1 682 31 4 1754

    6 Arunachal pradesh --- 0.5 2 1 87 90

    7 Jammu & Kashir 280 0.5 2 1 11 302

    8 Karnataka 480 410 0.5 336 131 1365

    9 Kerala 86 58 54 NA 30 228

    10 Madhya Pradesh 801 132 26 700 145 1804

    11 Maharastra 379 260 -- 1046 117 1802

    12 Manipur --- --- --- --- 65 65

    13 Meghalaya --- --- --- --- 37 37

    14 Orissa 655 233 NA 127 --- 1015

    15 Punjab 1383 -- 1559 172 7 3121

    16 Rajasthan 887 53 50 1219 30 2547

    17 Tamil nadu 911 750 62 807 35 2565

    18 Tripura --- 2 --- 0.5 23 30

    19 Uttar pradesh 2473 330 3189 1314 349 7933

    20 West Bengal 960 303 --- 17 209 1409

    21 Union Territores 28 3 45 7 35 118

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    All India 13775 3986 6469 7557 2304 34491

    NA = Not Available

    Source: Water Use Efficiency in Agriculture by S. Giriappa, P.35.

    Total ground water resources can irrigate 42.29 m ha, but present utilization is

    only 10.01 m ha and remaining 32.28 m ha is left unutilized, though there is a potential to

    explore it.

    VII. Economic Use of Water Resources

    Water is the most critical input in crop production. It also influences almost all the

    bio-physiological processes of plants. When we speak of economic use of water, it refers

    to the system which aims at optimum utilization of available water resources in crop

    production without adversely affecting soil health. As we have discussed earlier the main

    source of water for plant growth is irrigation, so while irrigating following important

    points are to be kept in mind. These are:

    --when to irrigate

    --how much to irrigate

    --how best to irrigate

    Determination of water requirement and criteria for scheduling irrigation help to

    define when to irrigate. The estimation of plant available moisture and deficit expressed

    as depth in the rooting zone enables to decide how much to irrigate. Selection of suitable

    method of irrigation in a given situation will meet the question how best to irrigate. Some

    other measures for efficient management of irrigation water are discussed as below.

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    Solution of the problem

    1. Check water logging

    It is one of the major problems in water management. The concept of plant

    available water capacity enables one to avoid application of excess water which further

    helps to minimize water- logging along with salinity and alkalinity. Frequent irrigations

    maintain high soil moisture regime but it depends on the method adopted for irrigation.

    2. Drainage

    To avoid water logging condition and salt accumulation, the field should be

    provided with a proper drainage system. The drainage provides suitable environment to

    the development of plant root system and helps in optimizing crop production.

    3. Disiltation of tanks

    Siltation of tanks and reservoirs both traditional and modem, has added to the

    gravity of problem of surface water management. It reduces the storage capacity of the

    reservoir or tanks and increases in the volume and velocity of floods. Disiltation may be

    difficult for the big reservoirs but this can be easily practised in tanks, ponds, ditches etc.

    4. Ground water management

    Management of surface water and ground water are equally important in water

    harvesting and recycling. In areas that greatly depend on ground water for their irrigation

    requirement, should be ensured that crops are provided with water during the critical

    period of their growth. For this exploitation of ground water should be managed in a

    balanced manner.

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    Total amount of precipitation received is constant, and its economical use is the

    only way to increase production. At present, 29% of the total precipitation is lost through

    surface run-off and 53% through infiltration. For better management of ground water, the

    ultimate aim is to increase from 53% of the total precipitation moving into the soil to 100

    per cent. This will recharge to ground water.

    Ground water availability gets considerably reduced due to increased exploitation

    and poor recharge conditions. Therefore, proper water balance between availability,

    recharge and exploitation should be maintained. For this, a proper study and planning is

    very necessary"

    5. Watershed management

    Watershed is the geographical area from which the entire surface run-off

    originating due to the rainfall coverage flows through the existing drainage system

    towards a common outlet Let us say, it is a small catchment area in which the excess

    water of that particular region resulting from run-off is conserved either by check darns or

    by gully plugs or through percolation ponds.

    An important planning input is watershed management is to conduct the ground

    water study. This study is undertaken to assess the ground water status, soil types and

    water stored at various depths. With this information it will be possible to plan properly

    the optimum utilization of the available water.

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    Conclusion

    The above discussion underlines the fact that in the face of anticipated population

    growth and technological advancement, the country's utilizable water resources are

    limited and there is no ground for complacency in the matter. There is utmost need for

    laying maximum emphasis on conservation and most efficient utilization of the available

    water resources. Technological and management capabilities will have to be upgraded for

    this purpose.

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    References

    www.indiawaterportal.com

    www.wbic.gov.in

    www.cwc.gov.in

    www.inseda.org

    http://www.indiawaterportal.com/http://www.indiawaterportal.com/http://www.wbic.gov.in/http://www.wbic.gov.in/http://www.cwc.gov.in/http://www.cwc.gov.in/http://www.inseda.org/http://www.inseda.org/http://www.inseda.org/http://www.cwc.gov.in/http://www.wbic.gov.in/http://www.indiawaterportal.com/