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Effects of soil organic matter components and iron aluminum oxides on aggregate stability during vegetation succession in granite red soil eroded areas

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Journal of Mountain Science 2022年第9期19卷 2634-2650页

作者： LIN Zhe HUANG Zhi-gang LIAO Da-lan HUANG Wan-xia HUANG Juan DENG Yu-song Guangxi Key Laboratory of Forest Ecology and Conservation College of ForestryGuangxi UniversityNanningGuangxi 530004China College of Agriculture Guangxi UniversityNanningGuangxi 530004China

soil aggregates determine the basic structure of soil,and their composition and stability are influenced by the various types of cementitious substances occurring in *** explore the main limiting factors of soil aggregation in the process of vegetation succession with granite as the parent material,five stages of vegetation succession in an eroded area were selected:bare land(BL),grassland(GL),grassland shrub transition land(GS),shrubland(SL)and secondary forest(SF).soil samples were collected to determine the composition and stability of *** contents of organic and inorganic cementitious substances,including organic matter components and iron aluminum oxides,were determined at five soil aggregate grain *** results indicated that the stability of soil aggregates and the>0.25 mm water-stable aggregate content(WR_(0.25))increased with vegetation *** on the Le Bissonnais(LB)method,the mean weight diameter(MWD)of soil aggregates increased,and the relative dissipation index(RSI)and relative mechanical crushing index(RMI)*** humic acid(HA)and fulvic acid(FA)contents in soil aggregates increased with vegetation succession,and the soil humus content at the SF stage increased by more than 13.54%over the BL *** different vegetation succession stage,the iron and aluminum oxides for the SL and the SF were at a high level,and the contents of free-form iron oxide(Fe_(d))and amorphous iron oxide(Fe_(o))for BL were *** analysis indicated that the soil humic degree(PQ)and the contents of amorphous alumina(Al_(o))were positively correlated with aggregate stability to varying *** analysis(RDA)revealed that PQ values of 1-2 mm(PQ_(2))and 0.25-0.5 mm(PQ_(4))aggregates,the contents of Fe_(o) of bulk soil(Fe_(oB)),>2 mm(Fe_(o1)),1-2 mm(Fe_(o2)),and2 mm(Al_(o1))aggregates could explain 99.4%of the changes in soil aggregate stability at different vegetati

关键词： soil aggregate stability Vegetation succession soil organic matter components Iron aluminum oxides

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