Development of Fe-rich clay minerals in a weathering profile derived from serpentinized ultramafic rock in Nui Nua massif, Vietnam-Reference-Cited by-同舟云学术

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Development of Fe-rich clay minerals in a weathering profile derived from serpentinized ultramafic rock in Nui Nua massif, Vietnam

Published:2017-12 Issue: Volume:308 Page:159-170
ISSN:0016-7061
Container-title:Geoderma
language:en
Short-container-title:Geoderma

Author:

Nguyen-Thanh Lan,Hoang-Minh Thao,Herbert Horst-Jürgen,Kasbohm Jörn,Lai Le Thi,Nguyen Minh Ngoc,Mählmann Rafael Ferreiro

Funder

National Foundation for Science and Technology Development

Publisher

Elsevier BV

Subject

Soil Science

Reference108 articles.

1. Soils and conifer forest productivity on serpentinized peridotite of the Trinity ophiolite, California;Alexander;Soil Sci.,1989

2. Determination of the cation exchange capacity of clays with Cu complex revisited;Ammann;Clay Miner.,2005

3. Formation of magnetite by bacteria and its application;Arakaki;J. Roy. Soc. Interface.,2008

4. Thermal enhancement of natural magnetism as a tool for tracing eroded soil;Armstrong;Earth Surf. Process. Landf.,2012

5. (Eds), Geological and Mineral Resources Map of Vietnam on 1:200.000 - Thanh Hoa E-48-IV Sheet - Map Explanation;Bach,1995

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