study of chemical and physical properties and the soil sorption of metolachlor and carbofuran in...
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Study of Chemical and Physical Properties and the Soil Sorption of Metolachlor and Carbofuran in Three Tropical SoilsTRANSCRIPT
Study of Chemical and Physical Properties and the Soil Sorption
of Metolachlor and Carbofuran in Three Tropical Soils
José A. Dumas, Peter Nkedi-Kizza and
Rafael Montalvo-Zapata
Organic Matter
ClayThe environmental fate of pesticides The environmental fate of pesticides
applied to soils is determined by sorption applied to soils is determined by sorption and degradation processes.and degradation processes.
The nature of organic matter will The nature of organic matter will determine soil aggregates as well as determine soil aggregates as well as pesticide sorption and degradation. pesticide sorption and degradation.
IntroductionTwo main soil components associated to Two main soil components associated to pesticide sorption are clay and organic matterpesticide sorption are clay and organic matter
Organic matter participates in translocation of micronutrients from the soil to the plant, enhances water retention, increases seed germination rates and percentages, and stimulates development of micro flora populations in soils. At the same time organic matter provides sorption surfaces for pesticides and other types of xenobiotics compounds.
Organic matter
Organic Matter – Humic and fulvic acids
Humic acid-pesticide interaction
Van der Waals and electrostatic interactions.
How pesticide’s sorption occurs?
Hypothesis
Chemical and physical properties of humic Chemical and physical properties of humic and fulvic acid are strongly different from and fulvic acid are strongly different from one soil type to another and hence affect one soil type to another and hence affect some pesticide interactions.some pesticide interactions.
Objectives
Characterize and compare chemical and Characterize and compare chemical and physical properties of three Puerto Rican physical properties of three Puerto Rican soils (two carbonatic soils and one organic soils (two carbonatic soils and one organic soil) soil)
Characterize the relationship of sorption of Characterize the relationship of sorption of metolachlor and carbofuran to organic metolachlor and carbofuran to organic matter properties in three tropical soilsmatter properties in three tropical soils
North Coastal Limestone Aquifer
South Coastal Alluvial Aquifer
Chemico-pharmaceutical industries
High urban development
Hydrogeographic (HP) map of Puerto Rico
Sampling areas and Soil Series Selected
TiburonesCatano
Aguilita
Methods Soils were collected from three or four point ons in each sampling Soils were collected from three or four point ons in each sampling
area from top to 60 cm depth.area from top to 60 cm depth. Samples were air dried, ground and sieved. Samples were air dried, ground and sieved. Characterization of soil physical and chemical propertiesCharacterization of soil physical and chemical properties
• pH, CEC, CaCOpH, CEC, CaCO3 3 content, organic carbon content content, organic carbon content (Walkley-Black method), particle size. (Walkley-Black method), particle size.
• Extraction of fat fraction, humic and fulvic acid content.Extraction of fat fraction, humic and fulvic acid content.• Characterization of humic and fulvic acid fraction by Characterization of humic and fulvic acid fraction by
derivative UV-Vis, and determination of E4/E6 ratio.derivative UV-Vis, and determination of E4/E6 ratio.• Determination of ATR-IR spectrum of humic and fulvic Determination of ATR-IR spectrum of humic and fulvic
acid fractions.acid fractions.• Determination of total acid content of humic and fulvic Determination of total acid content of humic and fulvic
acid fractionsacid fractions To develop sorption isotherms curves of metolachlor and carbofuran To develop sorption isotherms curves of metolachlor and carbofuran
(Batch slurry method).(Batch slurry method).
Soil properties
Soil Series
pH CCE
%
Clay
%
Silt
%
Sand
%
WHC
AguilitaAguilita 8.188.18 63.1363.13 47.6847.68 22.8822.88 29.4429.44 4545
CataCataññoo 8.608.60 14.0114.01 4.564.56 3.363.36 92.0892.08 2222
TiburonesTiburones 4.074.07 0.840.84 17.4417.44 2.842.84 79.7279.72 3838
CCE-Calcium carbonate equivalen; WHC-Water holding capacityt
Organic matter properties
Soil Series HA
mg1
FA
mg1
HA/FA OC
%
Fat
mg/kg OC
AguilitaAguilita 600600 590590 1.01.0 4.084.08 950950
CataCataññoo 2525 8484 0.30.3 0.530.53 161161
TiburonesTiburones 990990 490490 2.02.0 7.937.93 27302730
HA-humic acid; FA-fulvic acid; 1mg/50g soil; OC-organic carbon
Fulvic and Humic acid properties
Soil Series E4/E6 Total Acidity
(meq/g humic)
HA FA HA FA
AguilitaAguilita 5.55.5 10.010.0 1.41.4 2.82.8
CataCataññoo 4.94.9 6.56.5 NDND 0.440.44
TiburonesTiburones 3.23.2 10.410.4 1.61.6 3.23.2
E4/E6-absorbance ratio at 400 and 600 nm
Potentiometric tiltration of Fulvic acid
8
8.5
9
9.5
10
10.5
11
11.5
12
12.5
0 2 4 6 8 10 12 14 16 18
ml HCl 0.102 N
pH
Aguilita AF Tiburones AF Catano AF
-COOH
Phenolic OH
Potentiometric tiltration of Humic acid
6
7
8
9
10
11
12
13
0 2 4 6 8 10 12 14 16 18
ml 0.1022 N HCl
pH
pH Aguilita pH Catano pH Tiburones
Non clearly defined acidic group protons
Derivative spectrum of Humic acid (100ug/mL)
-1
-0.8
-0.6
-0.4
-0.2
0
0.2
0.4
0.6
0.8
1
200 250 300 350 400 450 500 550 600 650
-1
-0.8
-0.6
-0.4
-0.2
0
0.2
0.4
0.6
0.8
1
200 250 300 350 400 450 500 550 600 650
-1
-0.8
-0.6
-0.4
-0.2
0
0.2
0.4
0.6
0.8
1
200 250 300 350 400 450 500 550 600 650
Aguilita
Catano
Tiburones
Derivative spectrum of Fulvic acid (100ug/mL)
Aguilita
Catano
Tiburones
-0.6
-0.5
-0.4
-0.3
-0.2
-0.1
0
0.1
0.2
200 250 300 350 400 450 500 550 600 650
-0.6
-0.5
-0.4
-0.3
-0.2
-0.1
0
0.1
0.2
200 250 300 350 400 450 500 550 600 650
-0.6
-0.5
-0.4
-0.3
-0.2
-0.1
0
0.1
0.2
200 250 300 350 400 450 500 550 600 650
Main functional groups of Fulvic acids (β-humus) identified by ATR-IR
Aguiliita
Catano
Tiburones
Benzene rings
Hydroxy groupsAromatic C-H
Si-H
C=O
C-O
Main functional groups of Humic acids identified by ATR-IR
Aguiliita
Catano
Tiburones
Structure of pesticides
Metolachlor Carbofuran
Chloroacetanilide Carbamate
Chemical and physical properties of Metolachlor and
Carbofuran
Name Family Sol.(mg/
L)
Koc(mL/g)
Kow pKb
MET cloroacetanilide 530 200 2820 NA
CAR carbamate 700 14-160 17-26 NA
MET-metolachlor; CAR-carbofuran
Sorption isotherms for Metolachlor
R2
= 0.9478
R2
= 0.9747
R2
= 0.963
0.00
20.00
40.00
60.00
80.00
100.00
120.00
0 5 10 15 20 25
Ce (mg/L)
Cs
(mg/
Kg)
Catano Aguilita Tiburones
Soil sorption coefficient
Soil Series Metolachlor
Kd
AguilitaAguilita 3.63.6
CataCataññoo 1.21.2
TiburonesTiburones 9.39.3
ConclusionCarbofuran sorption coefficient for CataCarbofuran sorption coefficient for Catañño o
soil series was higher than that found for soil series was higher than that found for Tiburones or Aguilita soils and also higher Tiburones or Aguilita soils and also higher than the sorption value reported in than the sorption value reported in literature.literature.
Fulvic and Humic acid properties of Fulvic and Humic acid properties of CataCatañño series are different from those of o series are different from those of Tiburones and Aguilita series.Tiburones and Aguilita series.
Data suggest that nature of organic matter Data suggest that nature of organic matter is a primary factor to be considered for an is a primary factor to be considered for an adequate interpretation of sorption and adequate interpretation of sorption and desorption pesticide data.desorption pesticide data.
Conclusion
This project was funded by the TSTAR program. We appreciate the excellent technical support of Norma Corchado and Esteban Rivera from the Central Analytical Laboratory, without whose assistance this work could not have been conducted.
Acknowledgement