Mineral weathering and element cycling in soil-microorganism-plant system

被引：46

作者：

Zhu YongGuan ^{[1
,2
]}

Duan GuiLan ^{[2
]}

Chen BaoDong ^{[2
]}

Peng XinHua ^{[3
]}

Chen Zheng ^{[2
]}

Sun GuoXin ^{[2
]}

机构：

[1] Chinese Acad Sci, Inst Urban Environm, Key Lab Urban Environm & Hlth, Xiamen 361021, Peoples R China

[2] Chinese Acad Sci, Ecoenvironm Sci Res Ctr, State Key Lab Reg & Urban Ecol, Beijing 100085, Peoples R China

[3] Chinese Acad Sci, Inst Soil Sci, State Key Lab Soil & Sustainable Agr, Nanjing 210008, Jiangsu, Peoples R China

来源：

SCIENCE CHINA-EARTH SCIENCES | 2014年 / 57卷 / 05期

基金：

国家自然科学基金重大项目;

关键词：

soil; plant; microorganism; geobiology; ARBUSCULAR MYCORRHIZAL FUNGUS; ECTOMYCORRHIZAL FUNGI; LUPINUS-ALBUS; AGGREGATE STABILITY; RHIZOSPHERE; IRON; PHOSPHORUS; REDUCTION; ROOT; ACCUMULATION;

D O I：

10.1007/s11430-014-4861-0

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

Soil is an essential part of the critical zone, and soil-microbe-plant system serves as a key link among lithosphere, biosphere, atmosphere and hydrosphere. As one of the habitats with the richest biodiversity, soil plays a critical role in element biogeochemistry on the earth surface (weathered crust). Here we review the soil biological processes that are relevant to mineral weathering, element cycling, and transformation, with an emphasis on rock weathering mediated by soil microbes, plant root and the rhizosphere.

引用

页码：888 / 896

页数：9

共 71 条

[1] A model to predict soil aggregate stability dynamics following organic residue incorporation under field conditions [J].