Irrigation water quality effects on soil carbon fractionation and organic carbon dissolution and leaching in a semiarid calcareous soil

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10 Citations (Scopus)

Abstract

Irrigation water quality and soil organic matter content influence crop yields and soil properties such as salinity and soil particle aggregation. We used laboratory column and batch studies and soil carbon fractionation to study potential organic carbon (OC) losses from a Typic Torrifluvent with 0.79% total OC and 4.7% inorganic carbon ([IC] as carbonates). About 4% of the total OC fraction was determined to be water-soluble OC (SOC). Under saturated flow, a significant amount of SOC (20%-35%) was lost from this soil (Pima clay loam) with just two pore volumes of irrigation water. Sodium- and sulfate-rich waters and rainwater were up to twice as effective at releasing SOC as waters dominated by calcium and chloride ions. Not all OC losses can be attributed to well-known soil particle dispersive effects of sodium and rainwater. Soluble OC losses were also highly correlated to the progressive dissolution of the soil IC fraction. Water quality has a measurable impact on OC and IC losses from OC-poor carbonate-rich soils. Changes in irrigation water quality may increase OC leaching from the plow layer and favor increased denitrification and potentially carbon sequestration in and below the root zone of irrigated semiarid soils.

Original languageEnglish (US)
Pages (from-to)365-371
Number of pages7
JournalSoil Science
Volume174
Issue number7
DOIs
StatePublished - Jul 2009

Fingerprint

semiarid soils
calcareous soil
calcareous soils
soil carbon
irrigation water
leaching
fractionation
water quality
organic carbon
dissolution
irrigation
carbon
inorganic carbon
soil
rainwater
total organic carbon
sodium
carbonate
water
clay loam

Keywords

  • Inorganic carbon
  • Organic carbon
  • Salinity
  • Semiarid climate soil
  • Water quality

ASJC Scopus subject areas

  • Soil Science

Cite this

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title = "Irrigation water quality effects on soil carbon fractionation and organic carbon dissolution and leaching in a semiarid calcareous soil",
abstract = "Irrigation water quality and soil organic matter content influence crop yields and soil properties such as salinity and soil particle aggregation. We used laboratory column and batch studies and soil carbon fractionation to study potential organic carbon (OC) losses from a Typic Torrifluvent with 0.79{\%} total OC and 4.7{\%} inorganic carbon ([IC] as carbonates). About 4{\%} of the total OC fraction was determined to be water-soluble OC (SOC). Under saturated flow, a significant amount of SOC (20{\%}-35{\%}) was lost from this soil (Pima clay loam) with just two pore volumes of irrigation water. Sodium- and sulfate-rich waters and rainwater were up to twice as effective at releasing SOC as waters dominated by calcium and chloride ions. Not all OC losses can be attributed to well-known soil particle dispersive effects of sodium and rainwater. Soluble OC losses were also highly correlated to the progressive dissolution of the soil IC fraction. Water quality has a measurable impact on OC and IC losses from OC-poor carbonate-rich soils. Changes in irrigation water quality may increase OC leaching from the plow layer and favor increased denitrification and potentially carbon sequestration in and below the root zone of irrigated semiarid soils.",
keywords = "Inorganic carbon, Organic carbon, Salinity, Semiarid climate soil, Water quality",
author = "Artiola, {Janick F} and Walworth, {James L}",
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TY - JOUR

T1 - Irrigation water quality effects on soil carbon fractionation and organic carbon dissolution and leaching in a semiarid calcareous soil

AU - Artiola, Janick F

AU - Walworth, James L

PY - 2009/7

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N2 - Irrigation water quality and soil organic matter content influence crop yields and soil properties such as salinity and soil particle aggregation. We used laboratory column and batch studies and soil carbon fractionation to study potential organic carbon (OC) losses from a Typic Torrifluvent with 0.79% total OC and 4.7% inorganic carbon ([IC] as carbonates). About 4% of the total OC fraction was determined to be water-soluble OC (SOC). Under saturated flow, a significant amount of SOC (20%-35%) was lost from this soil (Pima clay loam) with just two pore volumes of irrigation water. Sodium- and sulfate-rich waters and rainwater were up to twice as effective at releasing SOC as waters dominated by calcium and chloride ions. Not all OC losses can be attributed to well-known soil particle dispersive effects of sodium and rainwater. Soluble OC losses were also highly correlated to the progressive dissolution of the soil IC fraction. Water quality has a measurable impact on OC and IC losses from OC-poor carbonate-rich soils. Changes in irrigation water quality may increase OC leaching from the plow layer and favor increased denitrification and potentially carbon sequestration in and below the root zone of irrigated semiarid soils.

AB - Irrigation water quality and soil organic matter content influence crop yields and soil properties such as salinity and soil particle aggregation. We used laboratory column and batch studies and soil carbon fractionation to study potential organic carbon (OC) losses from a Typic Torrifluvent with 0.79% total OC and 4.7% inorganic carbon ([IC] as carbonates). About 4% of the total OC fraction was determined to be water-soluble OC (SOC). Under saturated flow, a significant amount of SOC (20%-35%) was lost from this soil (Pima clay loam) with just two pore volumes of irrigation water. Sodium- and sulfate-rich waters and rainwater were up to twice as effective at releasing SOC as waters dominated by calcium and chloride ions. Not all OC losses can be attributed to well-known soil particle dispersive effects of sodium and rainwater. Soluble OC losses were also highly correlated to the progressive dissolution of the soil IC fraction. Water quality has a measurable impact on OC and IC losses from OC-poor carbonate-rich soils. Changes in irrigation water quality may increase OC leaching from the plow layer and favor increased denitrification and potentially carbon sequestration in and below the root zone of irrigated semiarid soils.

KW - Inorganic carbon

KW - Organic carbon

KW - Salinity

KW - Semiarid climate soil

KW - Water quality

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