A quantitative reconstruction of a loess-paleosol sequence focused on paleosol genesis: An example from a section at Chaoyang, China
详细信息 查看全文
- 作者：Zhong-Xiu Suna ; b ; sun19871001@126.com" class="auth_mail" title="E-mail the corresponding author ; Phillip R. Owensb ; prowens@purdue.edu" class="auth_mail" title="E-mail the corresponding author ; Chun-Lan Hana ; hancly@163.com" class="auth_mail" title="E-mail the corresponding author ; Hui Chena ; ch@fofcc.org.cn" class="auth_mail" title="E-mail the corresponding author ; Xiao-Lei Wanga ; Xiaolei2785@126.com" class="auth_mail" title="E-mail the corresponding author ; Qiu-Bing Wanga ; wangqbsy@yahoo.com" class="auth_mail" title="E-mail the corresponding author
- 关键词：Loess&ndash ; paleosol ; Paleoclimate ; Depositon ; Pedogenesis ; Reconstruction analysis
- 刊名：Geoderma
- 出版年：2016
- 出版时间：15 March 2016
- 年：2016
- 卷：266
- 期：Complete
- 页码：25-39
- 全文大小：2593 K
文摘
- •
Two quantitative reconstruction models were used to examine paleosol formation.
- •
Silt weathering and translocation were quantified as the main soil-forming process.
- •
The deposition of loess was synchronized with pedogenic processes.
- •
The formation of paleosol or loess depends on the relative rate of deposition and pedogenesis.