Organic carbon accumulation on soil mineral surfaces in paddy soils derived from tidal wetlands

网站地图 | English | 公务邮箱

About the library

Background
History
Leadership
Organization

Opening Hours
Collections
Help Via Email

Electronic Information Resources

Organic carbon accumulation on soil mineral surfaces in paddy soils derived from tidal wetlands

详细信息查看全文

作者：Livia Wissing^a ; ^{l.wissing@wzw.tum.de" class="auth_mail} ; Angelika Kö ; lbl^a ; ^{koelbl@wzw.tum.de" class="auth_mail} ; Peter Schad^a ; ^{schad@wzw.tum.de" class="auth_mail} ; Tino Brä ; uer^b ; ^{tbraeuer@leibniz.uni-kiel.de" class="auth_mail} ; Zhi-Hong Cao^c ; ^{zhihongcaoli@126.com" class="auth_mail} ; Ingrid Kö ; gel-Knabner^a ; ^d ; ^{koegel@wzw.tum.de" class="auth_mail}
关键词：Pedogenesis ; Chronosequence ; Paddy rice cultivation ; Iron oxides ; Specific surface area ; Decalcification
刊名：Geoderma
出版年：September 2014
年：2014
卷：228-229
期：Complete
页码：90-103
全文大小：779 K

文摘

•: No additional formation of mineral surfaces during 2000 years of soil development
•: Paddy soils are characterized by high OC coverage on mineral surfaces.
•: Non-paddy soils, in which decalcification was retarded, showed lower OC coverage.
•: Iron oxides and SOM protect each other in organo-mineral associations.
•: OC coverage by complex association between clay minerals, iron oxides and SOM

NGLC 2004-2010.National Geological Library of China All Rights Reserved.
Add:29 Xueyuan Rd,Haidian District,Beijing,PRC. Mail Add: 8324 mailbox 100083
For exchange or info please contact us via email.