Organic matter accumulation in size fractions of soils of the semiarid Argentina. Effects of climate, soil texture and management

HEVIA, G.; BUSCHIAZZO, D.E.; HEPPER, E.; URIOSTE, A.; ANTON, L.

GEODERMA

ELSEVIER SCIENCE BV

Año: 2003 vol. 116 p. 265 - 277

0016-7061

Soil organic matter contents (SOM) of soils of the Semiarid Pampas of Argentina (SAP), mostly Entic Haplustolls, increase with the amount of silt + clay, but it is still not known how soil texture affects its qualitative composition in interaction with climatic and management conditions. Because of that the organic matter content of the following aggregate size fractions were determined: < 2000 Am (SOM), 100–2000 Am (YOM), < 100 Am (HOM), water floatable organic matter (FOM), and the E4/E6 quotient. These fractions were studied in the 20-cm topsoils of seven REFERENCE (virgin Caldenal savanna-like soils), and 10 CULTIVATED soils (under continuous conventional tillage since more than 50 years). Results showed that SOM of both REFERENCE and CULTIVATED soils was mainly composed by YOM (57%), and to a lesser extent by HOM (37%) and FOM (5%). Silt + clay conditioned positively the contents of SOM, YOM and HOM of both REFERENCE (R2 = 0.18, R2 = 0.21, R2 = 0.21, respectively, n = 21, p < 0.05) and CULTIVATED soils (R2= 0.62, R2= 0.44, R2 = 0.52, respectively, n= 30, p < 0.001). The positive fulvic acids exist in the well humified organic fraction of the studied soils. Contents of FOM and E4/ E6 values did not correlated with the climatic conditions nor with soil texture or management. Potential SOM losses can be larger in fine-textured soils (up to 54.3 Mg C ha
1) than in coarsetextured (up to 35.7 Mg C ha
1). Probable changes of soil texture by wind erosion will modify absolute contents of SOM, YOM and HOM, while modifications of temperature or rains regimes will affect HOM more. relationship existing between silt + clay and both SOM and YOM seems to be not longer valid in
1) than in coarsetextured (up to 35.7 Mg C ha
1). Probable changes of soil texture by wind erosion will modify absolute contents of SOM, YOM and HOM, while modifications of temperature or rains regimes will affect HOM more. relationship existing between silt + clay and both SOM and YOM seems to be not longer valid in
1). Probable changes of soil texture by wind erosion will modify absolute contents of SOM, YOM and HOM, while modifications of temperature or rains regimes will affect HOM more. relationship existing between silt + clay and both SOM and YOM seems to be not longer valid inrelationship existing between silt + clay and both SOM and YOM seems to be not longer valid in sites with mean annual temperatures (MAT) higher than 17 jC. YOM and HOM accumulation were positively affected by precipitation and negatively by temperature in combination with silt + clay. This effect was more pronounced for HOM. The slopes of the regressions between SOM, HOM and YOM with silt + clay were more pronounced for REFERENCE soils than for CULTIVATED soils, indicating the largest absolute losses of these organic matter fractions in fine- rather than in coarsetextured soils. E4/E6 quotients were lower than 5 in all studied soils indicating that humic rather thanm (SOM), 100–2000 Am (YOM), < 100 Am (HOM), water floatable organic matter (FOM), and the E4/E6 quotient. These fractions were studied in the 20-cm topsoils of seven REFERENCE (virgin Caldenal savanna-like soils), and 10 CULTIVATED soils (under continuous conventional tillage since more than 50 years). Results showed that SOM of both REFERENCE and CULTIVATED soils was mainly composed by YOM (57%), and to a lesser extent by HOM (37%) and FOM (5%). Silt + clay conditioned positively the contents of SOM, YOM and HOM of both REFERENCE (R2 = 0.18, R2 = 0.21, R2 = 0.21, respectively, n = 21, p < 0.05) and CULTIVATED soils (R2= 0.62, R2= 0.44, R2 = 0.52, respectively, n= 30, p < 0.001). The positive fulvic acids exist in the well humified organic fraction of the studied soils. Contents of FOM and E4/ E6 values did not correlated with the climatic conditions nor with soil texture or management. Potential SOM losses can be larger in fine-textured soils (up to 54.3 Mg C ha
1) than in coarsetextured (up to 35.7 Mg C ha
1). Probable changes of soil texture by wind erosion will modify absolute contents of SOM, YOM and HOM, while modifications of temperature or rains regimes will affect HOM more. relationship existing between silt + clay and both SOM and YOM seems to be not longer valid in
1) than in coarsetextured (up to 35.7 Mg C ha
1). Probable changes of soil texture by wind erosion will modify absolute contents of SOM, YOM and HOM, while modifications of temperature or rains regimes will affect HOM more. relationship existing between silt + clay and both SOM and YOM seems to be not longer valid in
1). Probable changes of soil texture by wind erosion will modify absolute contents of SOM, YOM and HOM, while modifications of temperature or rains regimes will affect HOM more. relationship existing between silt + clay and both SOM and YOM seems to be not longer valid inrelationship existing between silt + clay and both SOM and YOM seems to be not longer valid in sites with mean annual temperatures (MAT) higher than 17 jC. YOM and HOM accumulation were positively affected by precipitation and negatively by temperature in combination with silt + clay. This effect was more pronounced for HOM. The slopes of the regressions between SOM, HOM and YOM with silt + clay were more pronounced for REFERENCE soils than for CULTIVATED soils, indicating the largest absolute losses of these organic matter fractions in fine- rather than in coarsetextured soils. E4/E6 quotients were lower than 5 in all studied soils indicating that humic rather thanCaldenal savanna-like soils), and 10 CULTIVATED soils (under continuous conventional tillage since more than 50 years). Results showed that SOM of both REFERENCE and CULTIVATED soils was mainly composed by YOM (57%), and to a lesser extent by HOM (37%) and FOM (5%). Silt + clay conditioned positively the contents of SOM, YOM and HOM of both REFERENCE (R2 = 0.18, R2 = 0.21, R2 = 0.21, respectively, n = 21, p < 0.05) and CULTIVATED soils (R2= 0.62, R2= 0.44, R2 = 0.52, respectively, n= 30, p < 0.001). The positive fulvic acids exist in the well humified organic fraction of the studied soils. Contents of FOM and E4/ E6 values did not correlated with the climatic conditions nor with soil texture or management. Potential SOM losses can be larger in fine-textured soils (up to 54.3 Mg C ha
1) than in coarsetextured (up to 35.7 Mg C ha
1). Probable changes of soil texture by wind erosion will modify absolute contents of SOM, YOM and HOM, while modifications of temperature or rains regimes will affect HOM more. relationship existing between silt + clay and both SOM and YOM seems to be not longer valid in
1) than in coarsetextured (up to 35.7 Mg C ha
1). Probable changes of soil texture by wind erosion will modify absolute contents of SOM, YOM and HOM, while modifications of temperature or rains regimes will affect HOM more. relationship existing between silt + clay and both SOM and YOM seems to be not longer valid in
1). Probable changes of soil texture by wind erosion will modify absolute contents of SOM, YOM and HOM, while modifications of temperature or rains regimes will affect HOM more. relationship existing between silt + clay and both SOM and YOM seems to be not longer valid inrelationship existing between silt + clay and both SOM and YOM seems to be not longer valid in sites with mean annual temperatures (MAT) higher than 17 jC. YOM and HOM accumulation were positively affected by precipitation and negatively by temperature in combination with silt + clay. This effect was more pronounced for HOM. The slopes of the regressions between SOM, HOM and YOM with silt + clay were more pronounced for REFERENCE soils than for CULTIVATED soils, indicating the largest absolute losses of these organic matter fractions in fine- rather than in coarsetextured soils. E4/E6 quotients were lower than 5 in all studied soils indicating that humic rather thanR2 = 0.18, R2 = 0.21, R2 = 0.21, respectively, n = 21, p < 0.05) and CULTIVATED soils (R2= 0.62, R2= 0.44, R2 = 0.52, respectively, n= 30, p < 0.001). The positive fulvic acids exist in the well humified organic fraction of the studied soils. Contents of FOM and E4/ E6 values did not correlated with the climatic conditions nor with soil texture or management. Potential SOM losses can be larger in fine-textured soils (up to 54.3 Mg C ha
1) than in coarsetextured (up to 35.7 Mg C ha
1). Probable changes of soil texture by wind erosion will modify absolute contents of SOM, YOM and HOM, while modifications of temperature or rains regimes will affect HOM more. relationship existing between silt + clay and both SOM and YOM seems to be not longer valid in
1) than in coarsetextured (up to 35.7 Mg C ha
1). Probable changes of soil texture by wind erosion will modify absolute contents of SOM, YOM and HOM, while modifications of temperature or rains regimes will affect HOM more. relationship existing between silt + clay and both SOM and YOM seems to be not longer valid in
1). Probable changes of soil texture by wind erosion will modify absolute contents of SOM, YOM and HOM, while modifications of temperature or rains regimes will affect HOM more. relationship existing between silt + clay and both SOM and YOM seems to be not longer valid inrelationship existing between silt + clay and both SOM and YOM seems to be not longer valid in sites with mean annual temperatures (MAT) higher than 17 jC. YOM and HOM accumulation were positively affected by precipitation and negatively by temperature in combination with silt + clay. This effect was more pronounced for HOM. The slopes of the regressions between SOM, HOM and YOM with silt + clay were more pronounced for REFERENCE soils than for CULTIVATED soils, indicating the largest absolute losses of these organic matter fractions in fine- rather than in coarsetextured soils. E4/E6 quotients were lower than 5 in all studied soils indicating that humic rather thanR2= 0.62, R2= 0.44, R2 = 0.52, respectively, n= 30, p < 0.001). The positive fulvic acids exist in the well humified organic fraction of the studied soils. Contents of FOM and E4/ E6 values did not correlated with the climatic conditions nor with soil texture or management. Potential SOM losses can be larger in fine-textured soils (up to 54.3 Mg C ha
1) than in coarsetextured (up to 35.7 Mg C ha
1). Probable changes of soil texture by wind erosion will modify absolute contents of SOM, YOM and HOM, while modifications of temperature or rains regimes will affect HOM more. relationship existing between silt + clay and both SOM and YOM seems to be not longer valid in
1) than in coarsetextured (up to 35.7 Mg C ha
1). Probable changes of soil texture by wind erosion will modify absolute contents of SOM, YOM and HOM, while modifications of temperature or rains regimes will affect HOM more. relationship existing between silt + clay and both SOM and YOM seems to be not longer valid in
1). Probable changes of soil texture by wind erosion will modify absolute contents of SOM, YOM and HOM, while modifications of temperature or rains regimes will affect HOM more. relationship existing between silt + clay and both SOM and YOM seems to be not longer valid inrelationship existing between silt + clay and both SOM and YOM seems to be not longer valid in sites with mean annual temperatures (MAT) higher than 17 jC. YOM and HOM accumulation were positively affected by precipitation and negatively by temperature in combination with silt + clay. This effect was more pronounced for HOM. The slopes of the regressions between SOM, HOM and YOM with silt + clay were more pronounced for REFERENCE soils than for CULTIVATED soils, indicating the largest absolute losses of these organic matter fractions in fine- rather than in coarsetextured soils. E4/E6 quotients were lower than 5 in all studied soils indicating that humic rather thanjC. YOM and HOM accumulation were positively affected by precipitation and negatively by temperature in combination with silt + clay. This effect was more pronounced for HOM. The slopes of the regressions between SOM, HOM and YOM with silt + clay were more pronounced for REFERENCE soils than for CULTIVATED soils, indicating the largest absolute losses of these organic matter fractions in fine- rather than in coarsetextured soils. E4/E6 quotients were lower than 5 in all studied soils indicating that humic rather than