Modelling of Soil Moisture Movement and Solute Transport in Parts of Malaprabha Command
Infiltration is one of the most important hydrological process through which water enters the soil surface and plays a significant role in controlling soil water storage, crop yields, irrigation efficiency and solute entry into the soil profile. In agriculture fields, generally, the top soils are en...
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description | Infiltration is one of the most important hydrological process through which water enters the soil surface and plays a significant role in controlling soil water storage, crop yields, irrigation efficiency and solute entry into the soil profile. In agriculture fields, generally, the top soils are enriched with high organic matter and clay, particularly in black soils that promotes sorption, biological degradation and transformation of contaminants. During the process some of the chemicals applied to farm land, move down with the deep percolating water from the root zone and there are likely chances to pollute the underlying ground water. Such instances are reported by locals in areas dominated by black soils of Malaprabha command area. In order to understand the extent of groundwater contamination through chemical fertilizers, insecticides and manures, two agricultural plots (sugarcane and banana plantation) have been identified in parts of Malaprabha command area covering parts of Saundatti, Ramdurg (Belagavi district) and Nargund taluks (Gadag district). Hydraulic properties such as infiltration and hydraulic conductivity were determined in the field. Soil samples were collected and analysed in the laboratory for texture and porosity. The study indicated that the soils of the region are layered in structure. Further, it is noticed that the coarse textured loamy soil is present below the fine textured soils (such as silty loam or clayey loam). Due to the presence of fine soils at the top, the irrigated water get accumulated and the evaporation takes place relatively faster and results in the accumulation of excess salt. It is also noticed that the layered soils have obvious effects on solute transport and salt accumulation in the clay rich soil layer at the interface. The average salt accumulation (Total Nitrogen) observed in the study area within soil profile is 18.7g/kg. The maximum salt accumulation (21.38 g/kg) occurred in the top layer of sugarcane plots followed by banana plantation (19.85 g/kg). It is also noticed that there are remarkable changes in the interlayered soils with reference to water infiltration characteristics and salt leaching intensities. Study revealed the fact that the properties of the soil profile with a silty loam interlayer is better than with a silty clay loam interlayer. |
doi_str_mv | 10.1007/s12594-021-1680-8 |
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K. ; Sujitha, Vidya ; Shivapur, Anand V. ; Tyagi, J. V.</creator><creatorcontrib>Purandara, B. K. ; Sujitha, Vidya ; Shivapur, Anand V. ; Tyagi, J. V.</creatorcontrib><description>Infiltration is one of the most important hydrological process through which water enters the soil surface and plays a significant role in controlling soil water storage, crop yields, irrigation efficiency and solute entry into the soil profile. In agriculture fields, generally, the top soils are enriched with high organic matter and clay, particularly in black soils that promotes sorption, biological degradation and transformation of contaminants. During the process some of the chemicals applied to farm land, move down with the deep percolating water from the root zone and there are likely chances to pollute the underlying ground water. Such instances are reported by locals in areas dominated by black soils of Malaprabha command area. In order to understand the extent of groundwater contamination through chemical fertilizers, insecticides and manures, two agricultural plots (sugarcane and banana plantation) have been identified in parts of Malaprabha command area covering parts of Saundatti, Ramdurg (Belagavi district) and Nargund taluks (Gadag district). Hydraulic properties such as infiltration and hydraulic conductivity were determined in the field. Soil samples were collected and analysed in the laboratory for texture and porosity. The study indicated that the soils of the region are layered in structure. Further, it is noticed that the coarse textured loamy soil is present below the fine textured soils (such as silty loam or clayey loam). Due to the presence of fine soils at the top, the irrigated water get accumulated and the evaporation takes place relatively faster and results in the accumulation of excess salt. It is also noticed that the layered soils have obvious effects on solute transport and salt accumulation in the clay rich soil layer at the interface. The average salt accumulation (Total Nitrogen) observed in the study area within soil profile is 18.7g/kg. The maximum salt accumulation (21.38 g/kg) occurred in the top layer of sugarcane plots followed by banana plantation (19.85 g/kg). It is also noticed that there are remarkable changes in the interlayered soils with reference to water infiltration characteristics and salt leaching intensities. Study revealed the fact that the properties of the soil profile with a silty loam interlayer is better than with a silty clay loam interlayer.</description><identifier>ISSN: 0016-7622</identifier><identifier>EISSN: 0974-6889</identifier><identifier>DOI: 10.1007/s12594-021-1680-8</identifier><language>eng</language><publisher>New Delhi: Geological Society of India</publisher><subject>Accumulation ; Agricultural land ; Agriculture ; Agrochemicals ; Biodegradation ; Chemical fertilizers ; Clay ; Clay loam ; Clay soils ; Contaminants ; Contamination ; Crop yield ; Earth and Environmental Science ; Earth Sciences ; Evaporation ; Fertilizers ; Geology ; Groundwater ; Groundwater pollution ; Hydraulic properties ; Hydrogeology ; Hydrology ; Infiltration ; Insecticides ; Interlayers ; Irrigation efficiency ; Layered soils ; Leaching ; Loam ; Moisture content ; Organic matter ; Percolating water ; Percolation ; Plantations ; Porosity ; Properties ; Root zone ; Salts ; Silt loam ; Soil ; Soil contamination ; Soil layers ; Soil moisture ; Soil porosity ; Soil profiles ; Soil properties ; Soil texture ; Soil water ; Soil water movement ; Soil water storage ; Solute transport ; Solutes ; Sugarcane ; Transport ; Water infiltration ; Water storage</subject><ispartof>Journal of the Geological Society of India, 2021-03, Vol.97 (3), p.293-296</ispartof><rights>Geol. 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V.</creatorcontrib><title>Modelling of Soil Moisture Movement and Solute Transport in Parts of Malaprabha Command</title><title>Journal of the Geological Society of India</title><addtitle>J Geol Soc India</addtitle><description>Infiltration is one of the most important hydrological process through which water enters the soil surface and plays a significant role in controlling soil water storage, crop yields, irrigation efficiency and solute entry into the soil profile. In agriculture fields, generally, the top soils are enriched with high organic matter and clay, particularly in black soils that promotes sorption, biological degradation and transformation of contaminants. During the process some of the chemicals applied to farm land, move down with the deep percolating water from the root zone and there are likely chances to pollute the underlying ground water. Such instances are reported by locals in areas dominated by black soils of Malaprabha command area. In order to understand the extent of groundwater contamination through chemical fertilizers, insecticides and manures, two agricultural plots (sugarcane and banana plantation) have been identified in parts of Malaprabha command area covering parts of Saundatti, Ramdurg (Belagavi district) and Nargund taluks (Gadag district). Hydraulic properties such as infiltration and hydraulic conductivity were determined in the field. Soil samples were collected and analysed in the laboratory for texture and porosity. The study indicated that the soils of the region are layered in structure. Further, it is noticed that the coarse textured loamy soil is present below the fine textured soils (such as silty loam or clayey loam). Due to the presence of fine soils at the top, the irrigated water get accumulated and the evaporation takes place relatively faster and results in the accumulation of excess salt. It is also noticed that the layered soils have obvious effects on solute transport and salt accumulation in the clay rich soil layer at the interface. The average salt accumulation (Total Nitrogen) observed in the study area within soil profile is 18.7g/kg. The maximum salt accumulation (21.38 g/kg) occurred in the top layer of sugarcane plots followed by banana plantation (19.85 g/kg). It is also noticed that there are remarkable changes in the interlayered soils with reference to water infiltration characteristics and salt leaching intensities. Study revealed the fact that the properties of the soil profile with a silty loam interlayer is better than with a silty clay loam interlayer.</description><subject>Accumulation</subject><subject>Agricultural land</subject><subject>Agriculture</subject><subject>Agrochemicals</subject><subject>Biodegradation</subject><subject>Chemical fertilizers</subject><subject>Clay</subject><subject>Clay loam</subject><subject>Clay soils</subject><subject>Contaminants</subject><subject>Contamination</subject><subject>Crop yield</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Evaporation</subject><subject>Fertilizers</subject><subject>Geology</subject><subject>Groundwater</subject><subject>Groundwater pollution</subject><subject>Hydraulic properties</subject><subject>Hydrogeology</subject><subject>Hydrology</subject><subject>Infiltration</subject><subject>Insecticides</subject><subject>Interlayers</subject><subject>Irrigation efficiency</subject><subject>Layered soils</subject><subject>Leaching</subject><subject>Loam</subject><subject>Moisture content</subject><subject>Organic matter</subject><subject>Percolating water</subject><subject>Percolation</subject><subject>Plantations</subject><subject>Porosity</subject><subject>Properties</subject><subject>Root zone</subject><subject>Salts</subject><subject>Silt loam</subject><subject>Soil</subject><subject>Soil contamination</subject><subject>Soil layers</subject><subject>Soil moisture</subject><subject>Soil porosity</subject><subject>Soil profiles</subject><subject>Soil properties</subject><subject>Soil texture</subject><subject>Soil water</subject><subject>Soil water movement</subject><subject>Soil water storage</subject><subject>Solute transport</subject><subject>Solutes</subject><subject>Sugarcane</subject><subject>Transport</subject><subject>Water infiltration</subject><subject>Water storage</subject><issn>0016-7622</issn><issn>0974-6889</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNp1kE1LxDAQhosouK7-AG8Bz9FJk-bjKItfsIuCKx5Dtp2uXdqmJq3gvzfLCp48zQvzPDPwZtklg2sGoG4iywsjKOSMMqmB6qNsBkYJKrU2xykDk1TJPD_NzmLcAUgBms-y95WvsG2bfkt8TV5905KVb-I4BUzhCzvsR-L6Kq3aaUSyDq6Pgw8jaXry4sIY997KtW4IbvPhyMJ3XeLPs5PatREvfuc8e7u_Wy8e6fL54Wlxu6QlZ3KkG17WQuXCodaqKKBSXGMpZGW4QzSCKWPAVaALVZaa4wYl40ygYaYuKyf5PLs63B2C_5wwjnbnp9CnlzYXxggoQKtEsQNVBh9jwNoOoelc-LYM7L4_e-jPpv7svj-rk5MfnJjYfovh7_L_0g8linKa</recordid><startdate>20210301</startdate><enddate>20210301</enddate><creator>Purandara, B. K.</creator><creator>Sujitha, Vidya</creator><creator>Shivapur, Anand V.</creator><creator>Tyagi, J. V.</creator><general>Geological Society of India</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H96</scope><scope>KR7</scope><scope>L.G</scope></search><sort><creationdate>20210301</creationdate><title>Modelling of Soil Moisture Movement and Solute Transport in Parts of Malaprabha Command</title><author>Purandara, B. K. ; Sujitha, Vidya ; Shivapur, Anand V. ; Tyagi, J. 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K.</au><au>Sujitha, Vidya</au><au>Shivapur, Anand V.</au><au>Tyagi, J. V.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Modelling of Soil Moisture Movement and Solute Transport in Parts of Malaprabha Command</atitle><jtitle>Journal of the Geological Society of India</jtitle><stitle>J Geol Soc India</stitle><date>2021-03-01</date><risdate>2021</risdate><volume>97</volume><issue>3</issue><spage>293</spage><epage>296</epage><pages>293-296</pages><issn>0016-7622</issn><eissn>0974-6889</eissn><abstract>Infiltration is one of the most important hydrological process through which water enters the soil surface and plays a significant role in controlling soil water storage, crop yields, irrigation efficiency and solute entry into the soil profile. In agriculture fields, generally, the top soils are enriched with high organic matter and clay, particularly in black soils that promotes sorption, biological degradation and transformation of contaminants. During the process some of the chemicals applied to farm land, move down with the deep percolating water from the root zone and there are likely chances to pollute the underlying ground water. Such instances are reported by locals in areas dominated by black soils of Malaprabha command area. In order to understand the extent of groundwater contamination through chemical fertilizers, insecticides and manures, two agricultural plots (sugarcane and banana plantation) have been identified in parts of Malaprabha command area covering parts of Saundatti, Ramdurg (Belagavi district) and Nargund taluks (Gadag district). Hydraulic properties such as infiltration and hydraulic conductivity were determined in the field. Soil samples were collected and analysed in the laboratory for texture and porosity. The study indicated that the soils of the region are layered in structure. Further, it is noticed that the coarse textured loamy soil is present below the fine textured soils (such as silty loam or clayey loam). Due to the presence of fine soils at the top, the irrigated water get accumulated and the evaporation takes place relatively faster and results in the accumulation of excess salt. It is also noticed that the layered soils have obvious effects on solute transport and salt accumulation in the clay rich soil layer at the interface. The average salt accumulation (Total Nitrogen) observed in the study area within soil profile is 18.7g/kg. The maximum salt accumulation (21.38 g/kg) occurred in the top layer of sugarcane plots followed by banana plantation (19.85 g/kg). It is also noticed that there are remarkable changes in the interlayered soils with reference to water infiltration characteristics and salt leaching intensities. Study revealed the fact that the properties of the soil profile with a silty loam interlayer is better than with a silty clay loam interlayer.</abstract><cop>New Delhi</cop><pub>Geological Society of India</pub><doi>10.1007/s12594-021-1680-8</doi><tpages>4</tpages></addata></record> |
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subjects | Accumulation Agricultural land Agriculture Agrochemicals Biodegradation Chemical fertilizers Clay Clay loam Clay soils Contaminants Contamination Crop yield Earth and Environmental Science Earth Sciences Evaporation Fertilizers Geology Groundwater Groundwater pollution Hydraulic properties Hydrogeology Hydrology Infiltration Insecticides Interlayers Irrigation efficiency Layered soils Leaching Loam Moisture content Organic matter Percolating water Percolation Plantations Porosity Properties Root zone Salts Silt loam Soil Soil contamination Soil layers Soil moisture Soil porosity Soil profiles Soil properties Soil texture Soil water Soil water movement Soil water storage Solute transport Solutes Sugarcane Transport Water infiltration Water storage |
title | Modelling of Soil Moisture Movement and Solute Transport in Parts of Malaprabha Command |
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