Influence of the addition of organic residues on carbohydrate content and structural stability of some highland soils in Ethiopia

. When over exploited and coupled with climatic conditions, tropical soils are subject to increased erosion and a loss of soil organic matter. Countermeasures include the incorporation of organic materials such as crop and animal residues. We studied the effect of adding crop residues and manure to...

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Published inSoil use and management Vol. 18; no. 4; pp. 404 - 411
Main Authors Spaccini, R., Piccolo, A., Mbagwu, J.S.C., Zena Teshale, A., Igwe, C.A.
Format Journal Article
LanguageEnglish
Published Oxford, UK Blackwell Publishing Ltd 01.12.2002
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Abstract . When over exploited and coupled with climatic conditions, tropical soils are subject to increased erosion and a loss of soil organic matter. Countermeasures include the incorporation of organic materials such as crop and animal residues. We studied the effect of adding crop residues and manure to soil, at five sites in Ethiopia, on carbohydrate properties, aggregate stability and the C and N distribution within water‐stable aggregates. The effects of organic amendments varied between sites. The largest content of carbohydrates was obtained in the control treatment at Holeta, Ginchi (90 kg ha–1 mustard meal), Jimma (5 t ha–1 cow dung + 9 t ha–1 coffee husk), Awassa (forested soil), and Sirinka (soil alley‐cropped with Leuceanae). The aggregate stability of these soils was highly correlated with the OM content but not with carbohydrates. The smaller aggregates (<1.00 mm) accumulated more carbohydrates than the larger (>1.00 mm), thereby suggesting a protecting effect within the finer soil fractions. A protecting role played by humified OM components was also indicated by the C and N distribution as well as the C:N ratios which showed preferential accumulation in small rather than in large aggregates. The isotopic 13C‐OC values of carbohydrate extracts were generally low, suggesting that OM was from plants with C3 photosynthetic pathways. Soil treatments with maize alone or combined with coffee husks at Jimma decreased the δ13C‰ values slightly, revealing that maize contributed a share of the labile OM. Despite the improvement in the soil OM content, neither the carbohydrate content nor the aggregate stability were increased to the level of the forested sites, suggesting that the additions of crop residues and manure were not alone sufficient to restore the soil physical quality.
AbstractList . When over exploited and coupled with climatic conditions, tropical soils are subject to increased erosion and a loss of soil organic matter. Countermeasures include the incorporation of organic materials such as crop and animal residues. We studied the effect of adding crop residues and manure to soil, at five sites in Ethiopia, on carbohydrate properties, aggregate stability and the C and N distribution within water‐stable aggregates. The effects of organic amendments varied between sites. The largest content of carbohydrates was obtained in the control treatment at Holeta, Ginchi (90 kg ha–1 mustard meal), Jimma (5 t ha–1 cow dung + 9 t ha–1 coffee husk), Awassa (forested soil), and Sirinka (soil alley‐cropped with Leuceanae). The aggregate stability of these soils was highly correlated with the OM content but not with carbohydrates. The smaller aggregates (<1.00 mm) accumulated more carbohydrates than the larger (>1.00 mm), thereby suggesting a protecting effect within the finer soil fractions. A protecting role played by humified OM components was also indicated by the C and N distribution as well as the C:N ratios which showed preferential accumulation in small rather than in large aggregates. The isotopic 13C‐OC values of carbohydrate extracts were generally low, suggesting that OM was from plants with C3 photosynthetic pathways. Soil treatments with maize alone or combined with coffee husks at Jimma decreased the δ13C‰ values slightly, revealing that maize contributed a share of the labile OM. Despite the improvement in the soil OM content, neither the carbohydrate content nor the aggregate stability were increased to the level of the forested sites, suggesting that the additions of crop residues and manure were not alone sufficient to restore the soil physical quality.
When over exploited and coupled with climatic conditions, tropical soils are subject to increased erosion and a loss of soil organic matter. Countermeasures include the incorporation of organic materials such as crop and animal residues. We studied the effect of adding crop residues and manure to soil, at five sites in Ethiopia, on carbohydrate properties, aggregate stability and the C and N distribution within water‐stable aggregates. The effects of organic amendments varied between sites. The largest content of carbohydrates was obtained in the control treatment at Holeta, Ginchi (90 kg ha –1 mustard meal), Jimma (5 t ha –1 cow dung + 9 t ha –1 coffee husk), Awassa (forested soil), and Sirinka (soil alley‐cropped with Leuceanae ). The aggregate stability of these soils was highly correlated with the OM content but not with carbohydrates. The smaller aggregates (<1.00 mm) accumulated more carbohydrates than the larger (>1.00 mm), thereby suggesting a protecting effect within the finer soil fractions. A protecting role played by humified OM components was also indicated by the C and N distribution as well as the C:N ratios which showed preferential accumulation in small rather than in large aggregates. The isotopic 13 C‐OC values of carbohydrate extracts were generally low, suggesting that OM was from plants with C3 photosynthetic pathways. Soil treatments with maize alone or combined with coffee husks at Jimma decreased the δ 13 C‰ values slightly, revealing that maize contributed a share of the labile OM. Despite the improvement in the soil OM content, neither the carbohydrate content nor the aggregate stability were increased to the level of the forested sites, suggesting that the additions of crop residues and manure were not alone sufficient to restore the soil physical quality.
Author Piccolo, A.
Igwe, C.A.
Mbagwu, J.S.C.
Zena Teshale, A.
Spaccini, R.
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Piccolo A Zena A & Conte P 1996. A comparison of acid hydrolysis for the determination of carbohydrates in soils. Communications in Soil Science and Plant Analysis 27, 2909-2915.
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Spaccini R Piccolo A Haberhauer G & Gerzabek MH 2000. Transformation of organic matter from maize residues into labile and humic fractions of three European soils as revealed by 13C distribution and CPMAS-NMR Spectra. European Journal Soil Science 51, 583-594.
Angers DA Recous S & Aita C 1997. Fate of carbon and nitrogen in water-stable aggregates during decomposition of 13C- and 15N-labelled wheat straw in situ. European Journal Soil Science 48, 295-300.
Piccolo A & Mbagwu JSC 1990. Effects of different organic amendments on soil aggregate stability and molecular sizes of humic substances. Plant and Soil 123, 27-37.
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Monreal CM Schulten, H-R & Kodama H 1997. Age, turnover and molecular diversity of soil organic matter in aggregates of a Gleysol. Canadian Journal Soil Science 77, 379-388.
Spaccini, R Zena, A Igwe, CA Mbagwu, JSC & Piccolo, A 2001. Carbohydrates in water-stable aggregates and particle size fractions of forested and cultivated soils in two contrasting tropical ecosystems. Biogeochemistry 53, 1-22.
Caron J Kay BD & Stone JA 1992. Improvement in structural stability of a clay loam with drying. Soil Science Society America Journal 56, 1583-1590.
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Tisdall JM & Oades JM 1982. Organic matter and water-stable aggregates in soils. Journal Soil Science 33, 141-163.
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References_xml – reference: Monreal CM Schulten, H-R & Kodama H 1997. Age, turnover and molecular diversity of soil organic matter in aggregates of a Gleysol. Canadian Journal Soil Science 77, 379-388.
– reference: Spaccini, R Zena, A Igwe, CA Mbagwu, JSC & Piccolo, A 2001. Carbohydrates in water-stable aggregates and particle size fractions of forested and cultivated soils in two contrasting tropical ecosystems. Biogeochemistry 53, 1-22.
– reference: Anderson JM & Ingram JSI eds 1993. Tropical soil biology and fertility. Handbook of Methods, 2nd ed, CAB International Wallingford..
– reference: Dalal RC & Mayer RJ 1988. Cultivation effects on carbohydrate contents of soil and fractions. Soil Science Society America Journal 52, 1361-1365.
– reference: Capriel P Beck T Borchert H & Harter P 1990. Relationship between soil aliphatic fraction extracted with supercritical hexane, soil microbial biomass, and soil aggregate stability. Soil Science Society America Journal 54, 415-420.
– reference: Piccolo A Zena A & Conte P 1996. A comparison of acid hydrolysis for the determination of carbohydrates in soils. Communications in Soil Science and Plant Analysis 27, 2909-2915.
– reference: Caron J Kay BD & Stone JA 1992. Improvement in structural stability of a clay loam with drying. Soil Science Society America Journal 56, 1583-1590.
– reference: Buyanovsky GA Aslam M & Wagner GH 1994. Carbon turnover in soil physical fractions. Soil Science Society America Journal 58, 1167-1173.
– reference: Lal R 1986. Conversion of tropical rainforests: potential and ecological consequences. Advances in Agronomy 39, 173-263.
– reference: Piccolo A Spaccini R Haberhauer G & Gerzabek MH 1999. Increased sequestration of organic carbon in soil by hydrophobic protection. Naturwissenschaften 86, 496-499.
– reference: Dutarte P Bartoli F Andreux F Portal JM & Ange A 1993. Influence of content and nature of organic matter on the structure of some sandy soils from West Africa. Geoderma 56, 459-478.
– reference: Spaccini R Piccolo A Haberhauer G & Gerzabek MH 2000. Transformation of organic matter from maize residues into labile and humic fractions of three European soils as revealed by 13C distribution and CPMAS-NMR Spectra. European Journal Soil Science 51, 583-594.
– reference: Piccolo A 2002. The supramolecular structure of humic substances. A novel understanding of humus chemistry and implications in soil Science. Advances in Agronomy 75,57-134..
– reference: Watts CW Whalley WR Longstaff DJ White RP Brooke PC & Whitmore AP 2001. Aggregation of a soil with different cropping history following the adition of organic materials. Soil Use and Management 17, 263-268.
– reference: Angers DA Recous S & Aita C 1997. Fate of carbon and nitrogen in water-stable aggregates during decomposition of 13C- and 15N-labelled wheat straw in situ. European Journal Soil Science 48, 295-300.
– reference: Piccolo A & Mbagwu JSC 1990. Effects of different organic amendments on soil aggregate stability and molecular sizes of humic substances. Plant and Soil 123, 27-37.
– reference: Fernandes ECM Motovalli PP Castilla C & Mukurumbira L 1997. Management control of soil organic matter dynamics in tropical land-use systems. Geoderma 79, 49-68.
– reference: Lichtfouse E Duo S Girardin C Grably M Balesdent J Behar F & Vandenbroucke M 1995. Unexpected 13C-enrichment of organic components from wheat crop soils: evidence for the in situ origin of soil organic matter. Organic Geochemistry 23, 865-868.
– reference: Desjardins T Volkoff B Andreux F & Cerri CC 1994. Organic carbon and 13C contents in soils and soil-size fractions, and their changes due to deforestation and pasture installation in Eastern Amazonia. Geoderma 61, 103-118.
– reference: Piccolo A & Mbagwu JSC 1999. Role of hydrophobic components of soil organic matter on soil aggregate stability. Soil Science Society America Journal 63, 1801-1810.
– reference: Tisdall JM & Oades JM 1982. Organic matter and water-stable aggregates in soils. Journal Soil Science 33, 141-163.
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Snippet . When over exploited and coupled with climatic conditions, tropical soils are subject to increased erosion and a loss of soil organic matter. Countermeasures...
When over exploited and coupled with climatic conditions, tropical soils are subject to increased erosion and a loss of soil organic matter. Countermeasures...
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istex
SourceType Enrichment Source
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StartPage 404
SubjectTerms crop residues
Ethiopia
manures
Soil amendments
soil organic matter
soil structure
stability
Title Influence of the addition of organic residues on carbohydrate content and structural stability of some highland soils in Ethiopia
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