Magnetic Difference Between Deep and Surface Soil Within an Agricultural Area in Southern China: Implications for Magnetic Mineral Transformation During Pedogenic Process Under Subtropical Climate-Reference-Cited by-同舟云学术

Magnetic Difference Between Deep and Surface Soil Within an Agricultural Area in Southern China: Implications for Magnetic Mineral Transformation During Pedogenic Process Under Subtropical Climate

Published:2020-10 Issue:10 Volume:7 Page:
ISSN:2333-5084
Container-title:Earth and Space Science
language:en
Short-container-title:Earth and Space Science

Author:

Ouyang Tingping¹²^ORCID,Li Mingkun¹^ORCID,Guo Yu³,Peng Shasha²,He Chenjian¹,Zhu Zhaoyu²

Affiliation:

1. School of Geography South China Normal University Guangzhou China

2. Key Laboratory of Ocean and Marginal Sea Geology, Guangzhou Institute of Geochemistry Chinese Academy of Sciences Guangzhou China

3. Geological Survey of Guangzhou Guangzhou China

Funder

National Natural Science Foundation of China

Guangzhou Science, Technology and Innovation Commission

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Environmental Science (miscellaneous)

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019EA001070

Reference96 articles.

1. Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years

2. Rock magnetic properties of lateritic soil profiles from southern India: Evidence for pedogenic processes

3. Magnetic susceptibility as a proxy for rainfall: Worldwide data from tropical and temperate climate

4. Climatic interpretation of the Luochuan and Lingtai loess sections, China, based on changing iron oxide mineralogy and magnetic susceptibility

5. Paleoclimatic forcing of magnetic susceptibility variations in Alaskan loess during the late Quaternary

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