土壤有机碳作用及转化机制研究进展
张维理1,KOLBEH2,张认连1
Research Progress of SOC Functions and Transformation Mechanisms
ZHANG WeiLi1,KOLBE H2,ZHANG RenLian1

图4. 土壤腐殖质形成土壤团聚体的两类模式[9,13]
A模式:土壤团聚体由长链的胡敏酸物质与土壤颗粒结合形成。B模式:土壤团聚体由腐殖化产生的多元化的短链物质构成,这些短链物质有多糖(黑色)、多肽(蓝色)、脂肪族化合物(绿色)和多环的木质素碎片(褐色)。这些短链物质通过阳离子(红色)与土壤矿物颗粒结合形成土壤团聚体

Fig. 4. Two models of soil aggregates formed with soil humus
A Model: Soil aggregates are formed by combination of long-chain humic acids with soil particles. B Model: Soil aggregates are composed of various short-chain substances produced by humification, such as polysaccharides (black), polypeptides (blue), aliphatic compounds (green) and polycyclic lignin fragments (brown). These short-chain substances are combined with soil mineral particles by cations (red) to form aggregates