Effect of soil organic carbon on unsaturated earth properties

Soil organic carbon (SOC) is a multifaceted and assorted combination of constituents. Due to anthropogenic actions, the earth’s SOC is lost, thus affecting soils various properties. The column and channel studies were conducted to evaluate the effect on the unsaturated earth properties by artificial...

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Veröffentlicht in:Environmental sustainability 2020-09, Vol.3 (3), p.267-278
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description Soil organic carbon (SOC) is a multifaceted and assorted combination of constituents. Due to anthropogenic actions, the earth’s SOC is lost, thus affecting soils various properties. The column and channel studies were conducted to evaluate the effect on the unsaturated earth properties by artificially entailing SOC using organic-based (natural/industrial) wastes. Natural decayed plant/ animal remains known as humus; industrial wastes like press mud, bagasse ash, and fly ash were used as the source of SOC to amend with four soils i.e. black cotton (BC), red, marshy and mountainous. Tests were designed based on response surface methodology through central composite rotatable design for five properties defined by the author as “Soil hydraulic property”—representing the effect of SOC on water holding capacity and hydraulic conductivity; “Soil perviousness property”-representing the effect of SOC on infiltration and porosity; “Soil aggregation property”—representing the effect of SOC on plasticity index and bulk density; “Soil and water conservation property”—representing the effect of SOC on erosion and runoff; “Soil stability property”—representing the effect of SOC on shrinkage limit and friability index. The developed, empirical models correlated humus for BC soil, bagasse ash for marshy soil, fly ash for red and mountainous soils, as the best soil-amendment combinations. Drained water quality was analyzed and the obtained results were within the tolerance limits, implying no harm to the quality of water seeping through amended earth.
doi_str_mv 10.1007/s42398-020-00113-1
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Drained water quality was analyzed and the obtained results were within the tolerance limits, implying no harm to the quality of water seeping through amended earth.</description><subject>Anthropogenic factors</subject><subject>Automation</subject><subject>Bagasse</subject><subject>Bulk density</subject><subject>Carbon</subject><subject>Climate change</subject><subject>Cotton</subject><subject>Decomposing organic matter</subject><subject>Design of experiments</subject><subject>Earth</subject><subject>Electron microscopes</subject><subject>Empirical analysis</subject><subject>Fly ash</subject><subject>Friability</subject><subject>Humus</subject><subject>Hydraulics</subject><subject>Industrial wastes</subject><subject>Influence</subject><subject>Marshes</subject><subject>Mountain soils</subject><subject>Mountains</subject><subject>Organic carbon</subject><subject>Organic soils</subject><subject>Particle size</subject><subject>Plasticity index</subject><subject>Porosity</subject><subject>Pressmud</subject><subject>Response surface methodology</subject><subject>Soil conservation</subject><subject>Soil erosion</subject><subject>Soil porosity</subject><subject>Soil properties</subject><subject>Soil shrinkage</subject><subject>Soil stability</subject><subject>Soil water</subject><subject>Soils</subject><subject>Unsaturated soils</subject><subject>Water conservation</subject><subject>Water quality</subject><subject>Water 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index</topic><topic>Porosity</topic><topic>Pressmud</topic><topic>Response surface methodology</topic><topic>Soil conservation</topic><topic>Soil erosion</topic><topic>Soil porosity</topic><topic>Soil properties</topic><topic>Soil shrinkage</topic><topic>Soil stability</topic><topic>Soil water</topic><topic>Soils</topic><topic>Unsaturated soils</topic><topic>Water conservation</topic><topic>Water quality</topic><topic>Water seepage</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Hugar, Guruprasad M.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Materials Science &amp; 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Due to anthropogenic actions, the earth’s SOC is lost, thus affecting soils various properties. The column and channel studies were conducted to evaluate the effect on the unsaturated earth properties by artificially entailing SOC using organic-based (natural/industrial) wastes. Natural decayed plant/ animal remains known as humus; industrial wastes like press mud, bagasse ash, and fly ash were used as the source of SOC to amend with four soils i.e. black cotton (BC), red, marshy and mountainous. Tests were designed based on response surface methodology through central composite rotatable design for five properties defined by the author as “Soil hydraulic property”—representing the effect of SOC on water holding capacity and hydraulic conductivity; “Soil perviousness property”-representing the effect of SOC on infiltration and porosity; “Soil aggregation property”—representing the effect of SOC on plasticity index and bulk density; “Soil and water conservation property”—representing the effect of SOC on erosion and runoff; “Soil stability property”—representing the effect of SOC on shrinkage limit and friability index. The developed, empirical models correlated humus for BC soil, bagasse ash for marshy soil, fly ash for red and mountainous soils, as the best soil-amendment combinations. 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subjects Anthropogenic factors
Automation
Bagasse
Bulk density
Carbon
Climate change
Cotton
Decomposing organic matter
Design of experiments
Earth
Electron microscopes
Empirical analysis
Fly ash
Friability
Humus
Hydraulics
Industrial wastes
Influence
Marshes
Mountain soils
Mountains
Organic carbon
Organic soils
Particle size
Plasticity index
Porosity
Pressmud
Response surface methodology
Soil conservation
Soil erosion
Soil porosity
Soil properties
Soil shrinkage
Soil stability
Soil water
Soils
Unsaturated soils
Water conservation
Water quality
Water seepage
title Effect of soil organic carbon on unsaturated earth properties
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