Laboratory validation of a resource quality-based conceptual framework for organic matter management

Organic resources (ORs) are essential inputs in tropical farming systems and their decomposition dynamics are related to their quality. A Decision Support System (DSS) for organic N management has been proposed earlier that subdivides ORs in four classes depending on their N, lignin, and soluble pol...

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Main Authors: Vanlauwe, Bernard, Gachengo, CN, Shepherd, Keith D., Barrios, E., Cadisch, Georg, Palm, Cheryl A.
Format: Journal Article
Language:Inglés
Published: Wiley 2005
Subjects:
Online Access:https://hdl.handle.net/10568/43627
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author Vanlauwe, Bernard
Gachengo, CN
Shepherd, Keith D.
Barrios, E.
Cadisch, Georg
Palm, Cheryl A.
author_browse Barrios, E.
Cadisch, Georg
Gachengo, CN
Palm, Cheryl A.
Shepherd, Keith D.
Vanlauwe, Bernard
author_facet Vanlauwe, Bernard
Gachengo, CN
Shepherd, Keith D.
Barrios, E.
Cadisch, Georg
Palm, Cheryl A.
author_sort Vanlauwe, Bernard
collection Repository of Agricultural Research Outputs (CGSpace)
description Organic resources (ORs) are essential inputs in tropical farming systems and their decomposition dynamics are related to their quality. A Decision Support System (DSS) for organic N management has been proposed earlier that subdivides ORs in four classes depending on their N, lignin, and soluble polyphenol contents. To validate this DSS, a 28-d aerobic incubation experiment was initiated with 32 ORs, mostly crop and tree residues, applied to a sandy loam soil. The ORs contained 1.4 to 53.2 g kg?1 of N, 25 to 295 g kg?1 of lignin, and 4 to 148 g kg?1 of soluble polyphenols. In vitro dry matter digestibility (IVDMD) ranged from 70 to 820 g kg?1 After 28 d, CO2–C production varied between 199 and 905 mg CO2–C kg?1 soil, and mineral N contents ranged from 5 to 109 mg N kg?1 soil. Based on N mineralization data, three classes of ORs were evident: Class A with N release > 0, Class B with N release approximately 0, and Class C with N release < 0 (N immobilization). Criteria to separate those classes were based on the OR N and polyphenol content and cut-off values between the classes agreed well with those proposed in the original DSS. For Class A ORs, N mineralization was negatively related to their lignin/N ratio (except for Gliricida residues) and for Class C ORs, N immobilization was positively related to their N content. Short-term mineralization data supported the existence of three classes of ORs instead of four originally proposed by the DSS. However, ORs also govern other functions, operating in the medium to long term, and for these functions, the original four-class concept may be proven valid.
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spelling CGSpace436272024-08-27T10:36:44Z Laboratory validation of a resource quality-based conceptual framework for organic matter management Vanlauwe, Bernard Gachengo, CN Shepherd, Keith D. Barrios, E. Cadisch, Georg Palm, Cheryl A. soil fertility soil organic matter organic fertilizers degradation fertilidad del suelo materia orgánica del suelo abonos orgánicos degradación Organic resources (ORs) are essential inputs in tropical farming systems and their decomposition dynamics are related to their quality. A Decision Support System (DSS) for organic N management has been proposed earlier that subdivides ORs in four classes depending on their N, lignin, and soluble polyphenol contents. To validate this DSS, a 28-d aerobic incubation experiment was initiated with 32 ORs, mostly crop and tree residues, applied to a sandy loam soil. The ORs contained 1.4 to 53.2 g kg?1 of N, 25 to 295 g kg?1 of lignin, and 4 to 148 g kg?1 of soluble polyphenols. In vitro dry matter digestibility (IVDMD) ranged from 70 to 820 g kg?1 After 28 d, CO2–C production varied between 199 and 905 mg CO2–C kg?1 soil, and mineral N contents ranged from 5 to 109 mg N kg?1 soil. Based on N mineralization data, three classes of ORs were evident: Class A with N release > 0, Class B with N release approximately 0, and Class C with N release < 0 (N immobilization). Criteria to separate those classes were based on the OR N and polyphenol content and cut-off values between the classes agreed well with those proposed in the original DSS. For Class A ORs, N mineralization was negatively related to their lignin/N ratio (except for Gliricida residues) and for Class C ORs, N immobilization was positively related to their N content. Short-term mineralization data supported the existence of three classes of ORs instead of four originally proposed by the DSS. However, ORs also govern other functions, operating in the medium to long term, and for these functions, the original four-class concept may be proven valid. 2005-07 2014-09-24T08:42:25Z 2014-09-24T08:42:25Z Journal Article https://hdl.handle.net/10568/43627 en Limited Access Wiley
spellingShingle soil fertility
soil organic matter
organic fertilizers
degradation
fertilidad del suelo
materia orgánica del suelo
abonos orgánicos
degradación
Vanlauwe, Bernard
Gachengo, CN
Shepherd, Keith D.
Barrios, E.
Cadisch, Georg
Palm, Cheryl A.
Laboratory validation of a resource quality-based conceptual framework for organic matter management
title Laboratory validation of a resource quality-based conceptual framework for organic matter management
title_full Laboratory validation of a resource quality-based conceptual framework for organic matter management
title_fullStr Laboratory validation of a resource quality-based conceptual framework for organic matter management
title_full_unstemmed Laboratory validation of a resource quality-based conceptual framework for organic matter management
title_short Laboratory validation of a resource quality-based conceptual framework for organic matter management
title_sort laboratory validation of a resource quality based conceptual framework for organic matter management
topic soil fertility
soil organic matter
organic fertilizers
degradation
fertilidad del suelo
materia orgánica del suelo
abonos orgánicos
degradación
url https://hdl.handle.net/10568/43627
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