Image from Google Jackets

Organic matter in termite mounds of the Brazilian cerrados

By: Contributor(s): Material type: ArticleArticleLanguage: English Description: p. 198-202Subject(s): LOC classification:
  • S 623 .S977
Online resources: In: In: Thomas, Richard J.; Ayarza, Miguel Angel (eds.). Sustainable land management for the oxisols of the Latin American savannas: Dynamics of soil organic matter and indicators of soil qualitySummary: This study assessed differences between soil organic matter (SOM) in termite mounds and that of surrounding clayey and loamy Oxisols in the Brazilian savannas, also known as the Cerrados. Samples were fractionated into clay (<2 micro m), silt (2-50 pm), and sand (50-250 micro m), and the fractions' SOM was characterized according to C, N, lignin, and carbohydrates. In the mounds, soil organic carbon (SOC) is enriched by a factor of 3.5 and 11.5 in the clayey and loamy Oxisols, respectively. Especially in the sand fraction, the SOC accumulated as particulate SOM. However, in all size fractions, we found higher lignin contents, lower ratios of acids to aldehydes of lignin-derived phenols, and lower ratios of microbial to plant-derived monosugars than in the fractions of the surrounding soil. These findings suggest that the SOM of the mounds is less decomposed.
Tags from this library: No tags from this library for this title.
Star ratings
    Average rating: 0.0 (0 votes)
Holdings
Item type Current library Collection Call number Copy number Status Date due Barcode Item holds
Books Books CIAT Library General Book Collection General Book Collection S 623 .S977 (Browse shelf(Opens below)) c.1 Available
Total holds: 0

Edited by Richard Thomas, Miguel A. Ayarza

This study assessed differences between soil organic matter (SOM) in termite mounds and that of surrounding clayey and loamy Oxisols in the Brazilian savannas, also known as the Cerrados. Samples were fractionated into clay (<2 micro m), silt (2-50 pm), and sand (50-250 micro m), and the fractions' SOM was characterized according to C, N, lignin, and carbohydrates. In the mounds, soil organic carbon (SOC) is enriched by a factor of 3.5 and 11.5 in the clayey and loamy Oxisols, respectively. Especially in the sand fraction, the SOC accumulated as particulate SOM. However, in all size fractions, we found higher lignin contents, lower ratios of acids to aldehydes of lignin-derived phenols, and lower ratios of microbial to plant-derived monosugars than in the fractions of the surrounding soil. These findings suggest that the SOM of the mounds is less decomposed.

Powered by Koha