土壤水分
土壤有机质
环境科学
有机质
地球科学
浸出(土壤学)
土壤科学
地质学
生态学
生物
作者
Martha Lustosa Carvalho,Victor Ferreira Maciel,Ricardo de Oliveira Bordonal,João Luís Nunes Carvalho,Tiago Osório Ferreira,Carlos Eduardo Pellegrino Cerri,Maurício Roberto Cherubin
标识
DOI:10.36783/18069657rbcs20220130
摘要
ABSTRACT Soils are the largest terrestrial carbon (C) reservoir, and most of this C is retained as soil organic matter (SOM). Due to its ability to capture, stabilize, and store C for extended periods, soils are considered important allies in decarbonizing the atmosphere. The term ‘C stabilization’ includes a series of mechanisms or processes by which soil C is protected within soils and its losses are reduced through microbial decomposition or leaching. Due to their relevance in the global C cycle, C stabilization mechanisms have received intensive attention from the scientific community. As new analytic technologies push the boundaries of what was previously possible to know, new paradigms emerge. This literature review summarizes the current knowledge of the main mechanisms that may promote SOM stabilization. Factors that govern accumulation of SOM are also addressed. We highlight the role of organo-mineral associations and spatial inaccessibility of SOM due to occlusion within soil aggregates to understand the relative contribution of these mechanisms in different soil conditions (e.g., soil texture, mineralogy, and land- use). In addition, the contribution of cutting-edge approaches and analytical techniques to advance the understanding of SOM protection is presented. Modern techniques to evaluate SOM on a micro, nano, and molecular scale can contribute to the mechanistic understanding of SOM stabilization and the study and adoption of management strategies that maintain and increase C stocks in soils.
科研通智能强力驱动
Strongly Powered by AbleSci AI