is 10317 (1982): guide for evaluation of soil properties ... · national environmental engineering...
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है”ह”ह
IS 10317 (1982): Guide for evaluation of soil propertiesrelevant to irrigation [FAD 17: Farm Irrigation andDrainage Systems]
Gr 3
IS : 10317 • 1982
Ifzdiafl StandardGUIDE FOR
EVALUATION OF SOIL PROPERTIESRELEVANT TO IRRIGATION
{JJ)( ~ 611·41 : ())] h7
® COp"yright 1983
INDIAN STANDARDS INSTITUTIONMANAK DIIAVAN. 9 HAIIAl>lJR suxu ZAFI\U. l\l/\RG
NE\V DELIII 110002
January 1983
IS : 10317 • 1982
IS : 10317 - 1982
Indian StandardGUIDE FOR
BVALUATION OF SOIL PROPERTIESRELEVANT TO IRRIGATION
Water Requirements for Crops Sectional Committee, AFDC 46
Chairma11
DR I. P. AnnOLRepresenting
Central Soil Salinity Research Institute (leAR),Kamal
of
of
or
( Government
( GovernmentDepartment of AgricultureKarnataka ), Bangalore
Gujarat Agricultural University, AhmadabadHaryana Agricultural University, HissarPunjab Agricultural University, LudhianaDepartment of Agriculture (Government
Rajasthan), Jaipur
Department of Agriculture (Government ofPunjab ), Chandigarh
Department of Agriculture ( Government ofHaryana ), Chandigarh
Department of Agriculture (Government ofMaharashtra ), Pune
Central Arid Zone Research In~titut~)Jodhpur
Department of Irrigation (Mini~try of Agriculture&. Irrigation ), New Delhi
MembersSURI SWARAN SINGH BA INS
SBRI SAT PAl.. BANSAl,
SImI S. K. Bnzuux
DR R. P. DRIlt8H!"I V. S. DINKAH
DR G. S. SHEKAWAT (AlI,rnal,)DR S. L. PANDAY Indian Agricultural Research Institute, New Delhi
DH N. P. SINGH ( Alternat' )Da B. D. PATHAK Central Ground Water Board, LucknowSImI G. H. SHANK..\R REDDY Andhra Pradesh Agricultural University, Hyderabad
DR A. VENKATAClIARY ( AltlNlale )
SURI P. K. KOCIIAU ( Alurnat» )JOINT DIRECTOR OF AORICULTURE Department of Agriculture
Gujarat ), AhmadabadAGRONOMIST ( IRRIGATE))
AGRIOUL'I'URE ) i Alternat« )JOINT DIREVTOR OJ' AGRICULTUR}~
( SOIL CONSERVATION)DEPUTY DIRECTOR 01' AORI
OULTURE (WATER USESPEO} ALITIRS ) ( Alt,rnate )
DR R. S. JOSHIDB S. S. KHANNADR S. D. KltFPARDR U. R. MEHTA
( Continued on pag, 2 )
@ CopyrIght 1983INDIAN STANDARDS INSTITUTION
This publication is protected under the Indian Copyright Act ( XIV of 1957 ) andreprottuctjon in whole or in part by any mean!' except with written permission of thepublisher aball be deemed to be an infringement of copyright under the laid Act.
Mimi",DB G. B. SHENDB
II. 10317 • 1982
( Cora,inued/rom Ifll' 1 )
R,p",,,,,.,National Environmental Engineering Research
Institute, NalPurDR H. G. SINOH University of Udaipur, UdaipurDR.P. S. TOMER National Dairy Research Institute (leAR), KarnalDB N. K. UMRANI Mahatma Phule Krtshi Vidyape~th, Rahuri8111U C. V. J. VAIUIA Central Board of Irrigation and Power, New Delhi
SHRI R. R AJARAMAN ( Alt"nat, )SHRI T. PUHNANANDAK, Director General, lSI (&-offieio Memb,,)
Director ( Agri & Food )
S,crltarySHRI V. S. MATHUR
Deputy Director ( Agri & Food), lSI
2
AMENDMENT NO. 1 APRIL 1984TO
15:10317-1982 GUIDE FOR EVALUATION OF SOILPROPERTIES RELEVANT TO IRRIGATION
£'0rri9~n!!.u!!l
(Page 6. ol.auee 2.4.3, against 81, No.1) Substitute t Less t'han 1.3 t fol' 'Less than 1.2'.
(AFDC 58)
Reprography Unit, lSI, New Delhi, India
IS : 10317 - 1982
Indian StandardGUIDE FOR
EVALUATION OF SOIL )lROPERTIESRELEVANT TO IRRIGATION
o. FOREWORD
0.1 This Indian Standard was adopted by the Indian Stannard.Institution on 25 October 1982, after the draft finalized by the WaterRequirements for Crops Sectional Committee had been approved by theAgricultural and Food Products Division Council.
0.2 Irrigation water plays a vital role in many soil process. The mannerin which water is distributed within the soil mass depends to a considerable extent on the individual soil properties.
0.3 In rating land for irrigation ( agriculture ), first attention should begiven to physical condition which make the land adoptable to carefulcontrol of moisture. Freedom from undesirable chemical characteristicsreceives second consideration and third, the soil properties which effectthe inherent productivity are to be considered.
O.f It is hoped that this guide would help in deciding the method ofirrigation, suitable crops for the area in relation to efficient utilization ofwater. This would also be useful to planners in selecting site forirrigation projects.
0.5 For the purpose of deciding whether a particular requirement of thisstandard is complied with, the final value, observed or calculated, expresling the result of a telt or analysis, shall be rounded off in accordancewith IS : 2-1960·, The number of significant places retained in therounded off value should be the same as that of the specified value in thisItandard.
1. SCOPE
1.1 This standard gives guidelines for evaluation of soil properties inrelation to irrigation.
-R.ulel tor roundln. offnumericalvalues ( rllJisM ).
3
Texture
Sandy loam to clay loamLoamy sand and claySand and claySand and clayAny texture
IS I 10317 • 1982
2. PHYSICAL PROPERTIES
2.1 Testare
2.1.1 Texture is an expression to indicate the coarseness or fineness ofthe soil as determined by the relative proportion of the various sizedprimary particles in the soil mass. It is one of the fundamental andpermanent characteristics that has direct bearing on structure, porosityadhesion and consistency. Sandy soils of open characters possess gooddrainage and aeration and are usually loose and friable and easy tohandle in tillage operation. Clayey and silty soils owing to have largesurface area possess high absorbtive and retention capacity for moisture.They usually have fine pores, are moderate to poor in drainage andaeration and are relatively difficult to handle for cultivation purpose.Proforma for land irrigability classes has also been mentioned inAppendix A.
2.1.2 The standards followed for soil Irrigability classes are mentionedbelow:
SoilI,rigability Class
ABCDNon-irrigable class
2.1.3 Basis for above classification of soil texture are given in Table 1.
2.2 Etrectlve Soil Depth
2.2.1 Soil depth modifies to a great extent the rooting system of plantswhich is ultimately reflected in irrigation, crop growth and yield.
2.2.2 The standards followed for effective soil depth in soil irrigabilityclassification are as under:
SoiII"igability CltUS
ABCDNon-irrigable loil class
4
EJfectivI Depth in mm
More than 900450 to 900225 to 45075 to 225
Less than 75
IS t 10317 • 1_
TABLE I BASIS FOR CLASSDlCATION FOR TEXTURE( CI.,u, 2.1.S )
Sf. 'I'm 01' CLASltJ'ICATION TBXTURJC SYMBOL RAlf'OB Dr POCBM'TNo. SOIL OF SOIL
,--_.__-A____-.-..
Sand Silt Clay
(I) (2) (3) (4) (5) (6) (7) (8)
i) Sandy Coarse Sanda s 99·100 ().f 0-18soils Loamy Is 63-92 5-25 0,,12
.nds
Ii) Loamy Moderately Sandy loam II 70·92 Q-lS 9..20soils course Fine aandy fil
loam
Medium Very fine IJljlsandy loam
-Loam I 50·70 10-25 10-26- Silt loam IiI 25·75 25·50 0-26-Silt si 0-50 50-100 ()'26
Moderately Sandy clay scI 65-85 0-13 17-30fine loam
Clay loam c' 35-70 8-25 21-40Silty clay s;&1 o.-.a 23-74- 25·.w
Joam
iii) Clayey Fine - Sandy clay sc 50-75 0-8 26·50soils - Silty clay sk 0-35 25-60 40-75
-Clay ~ 0·62 0-25 '2-100
2.3 IDfiltratloD
2.3.1 Infiltration is the downward entry of water into the soil. It isthe maximum rate at which a soil in a given condition at given time eanabsorb rain or irrigation water. It is classified as below:
Class Buic Infilteratioll Raumm/Hour
1. Very ,10\\' Less than 0'25 em/hour to 2'52. Slow 2'5 to 12'53. Moderate 12·5 to 254. Rapid More than 25
2.3.2 Infiltration is a dynamic and quite variable character of soil andcan be fairly well controlled by management practices.
5
D
c
Soil Irrigabiliry Class
AB
IS : 10317 • 1982
2.4 Permeability
2.4.1 Permeability are of two types (i) Qualitative (ii) Quantitative.
2.4.1.1 Qualitative - The quality or state of porous medium relativeto the readyness with which such a medium conducts or transmit fluids.
2.4.1.2 OJlantitative - The specific properties governing the rate orreadyness with which a porous medium transmits fluid under standardposition.
2.4.2 The permeability depends upon pore size distribution of the soil.Texture and structure of a soil often studied in field for qualitativeassessment of permeability. Concentration and composition of saltsdissolved in irrigation water also effect the permeability of soils.
2.4.3 The degree of permeability may be distinguished as follows:
Permeability Class mmlhour
'I. Very slow Less than 1·22. Slow 1·3 to 53. Moderately slow 5 to 204. Moderate 20 to 505. Moderately rapid 50 to 1306. Rapid 130 to 2507. Very rapid Above 250
2.4.4 The standards followed for permeability for soil irrigability classare as under:
Permeabilib' mm/hour
5 to 501·3 to 550 to 1300·3 to 1·3130 to 250Less than 0·3 and
greater than 250
Soil permeability as a criteria is not applicable to deep black soilbecause of their unique properties. Deep black soils ( vertisols) whichare inherently slowly permeable due to expanding 2: 1 lattic type mineralsdo not qualify for irrigability class-A, they would qualify for B, C 8t DClass.
6
IS : 10317 • 1982
2.5 Drainage
2.5.1 The processes of discharge of water from an area of soil by sheetor stream; flow ( surface drain ige ) and removal of excess water fromwithin soil by downward flow through the soil ( internal drainage).Generally speaking coarse texture soil drain better than fine texture soil.Drainage depends directly on permeability of soil.
2.5.2 Standards followed for drainage for irrigahility class arc a~ below:
1\ an 1 B Class I 40VVer subsoil is at least moderately permeable01' permeable layer of at lea-t fi inch thicknessoccurs immediately below soil but within 10feet ( sand and gravels ).
(~ and D Class Moderately permeable subsoil or other perme-ahle layer of at least 6 inch thickness occurswith depth of 10 metres.
2.6 Soil TelDperature
2.6.1 Soil temperature has extensive effect on soil properties andbehaviour. The water holding capacity of soil decreases slightly withrise in temperature. Soil moisture is the most vital controlling factor insoil temperature.
3. CRITERIA FOR CLASSIFICATION
3.1 Criteria for classification of soil on the basis of properties ( see 2 ) aregiven in "fable 2.
7
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utle
ts
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eded
._
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ate
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in-
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ve-
age
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ay(
null
alo
ped
orri
ver
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ura
ld
rain
age
ou
tlet
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aila
ble:
cost
of
pu
mp
off
dra
inag
eex
ceed
__
Rs
ha
4.D
epth
of
Mo
reth
an5
wat
erta
ble
met
res
3·0-
5m
etre
s1·
5-3
met
res
1·5
met
res
and
belo
w
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hre
gar
dto
item
su
nd
erT
op
og
rap
hy
(2)
and
Dra
inag
e(2
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d(3
)th
ecr
rtcr
ra'\
'1))
hav
eto
bew
orke
dou
tfo
rea
chp
roje
cton
the
basi
so
floc
alco
ndit
ions
.
.... rll ... e ... ~ .. ~ =
INTERNATIONAL SYSTEM Of UNITS ( 51 UNITS)
".VaJta
Q,UAJrTITY UNIT SYMJjoL
Length metre m
Mau kilogram kg
Time second
Electric current ampere A
Thermodynamic kf~lvin Ktemperature
Luminous inlenaity candela cd
Amount of substance mole mol
hpplemeatary VDit.
QUANTITY UNIT SYMBOL
PJaue angle radian rad
Solid anile steradian sr
Derived UDit.
QUAMTI'l'Y UNa'. SYMBOL DIt;lI'INI'I'IUN
Force newton N N == 1 ks.m/t'Energy joule J J == 1 N.mPower watt W 1 W == 1 J/sFlux weber Wb I Wb = 1 v.,Flux density tesla T I T = 1 Wb/rn-Frequency hertz Hz J Hz = 1 cis (5- 1;
Electric conductance siemens S I S = 1 A/VElectromotive force volt V 1 V = 1 W/APr.ure, stress pascal Pa 1 Pa = t N/m'
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