中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Physical weathering of Gobi Desert sediments under different temperature and humidity conditions

文献类型:期刊论文

作者Wang, Xunming1,2; Zhu, Bingqi2; Wang, Zhenting3; Zhang, Caixia3; Geng, Xin2; Han, Likun2; Zheng, Yang2; Cai, Diwen2; Li, Danfeng2
刊名CATENA
出版日期2024
卷号234页码:12
ISSN号0341-8162
关键词Physical weathering Temperature Moisture Grain size Gobi Desert
DOI10.1016/j.catena.2023.107597
通讯作者Li, Danfeng(lidf@igsnrr.ac.cn)
英文摘要Physical weathering of the Gobi Desert surface sediments involves complex processes. However, our understanding of its main driving factors is still limited, and experimental observations on the weathering intensity of Gobi Desert surface sediments under changing environmental conditions are still insufficient. Surface samples were collected from the Gobi Desert, divided into 0.063-0.125 mm, 0.125-0.25 mm, 0.25-0.5 mm, 0.5-1 mm and 1-2 mm groups, and washed with deionized water. Physical weathering and salt weathering experiments of these groups were conducted under temperature (T) of -40 degrees C-40 degrees C and relative humidity (RH) of 20 %-100 %. Salt and mineral analyses, grain size distribution, and morphology analysis of each fraction group before and after the experiments were conducted. The results showed that mean grain sizes for the 0.063-0.125 mm, 0.125-0.25 mm, 0.25-0.5 mm, 0.5-1 mm, and 1-2 mm groups decreased by 0.49 +/- 1.09 %, -0.27 +/- 2.14 %, 0.41 +/- 3.14 %, 2.96 +/- 3.14 %, and 0.19 +/- 1.29 %, respectively. The mean size of each group decreased similar to 0.76 +/- 1.13 % /10 days, demonstrating a higher physical weathering intensity than the previous estimations. The d(0.1) size (i.e., the grain diameter for which 0.1 % of each grain group is smaller) was more sensitive to physical weathering, and the skewness was a good indicator of physical weathering for groups obeying a normal distribution. Physical weathering was still affected by salt weathering, and there was no regular pattern for physical weathering under variations in salt and mineral contents. At present, there are still difficulties in developing an accurate physical weathering intensity model.
WOS关键词CENTRAL NAMIB DESERT ; LABORATORY SIMULATION ; THERMAL-EXPANSION ; CARBONATE ROCKS ; SOIL PRODUCTION ; FREEZE-THAW ; MOISTURE ; RATES ; EVOLUTION ; PROPAGATION
资助项目National Natural Science Foundation of China[41930640] ; Key Frontier Program of Chinese Academy of Sciences[QYZDJ-SSWDQC043]
WOS研究方向Geology ; Agriculture ; Water Resources
语种英语
出版者ELSEVIER
WOS记录号WOS:001107941300001
资助机构National Natural Science Foundation of China ; Key Frontier Program of Chinese Academy of Sciences
源URL[http://ir.igsnrr.ac.cn/handle/311030/200527]  
专题中国科学院地理科学与资源研究所
通讯作者Li, Danfeng
作者单位1.Univ Chinese Acad Sci, Coll Resources & Environm, Beijing 100049, Peoples R China
2.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
3.Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Key Lab Desert & Desertificat, Lanzhou 730000, Peoples R China
推荐引用方式
GB/T 7714
Wang, Xunming,Zhu, Bingqi,Wang, Zhenting,et al. Physical weathering of Gobi Desert sediments under different temperature and humidity conditions[J]. CATENA,2024,234:12.
APA Wang, Xunming.,Zhu, Bingqi.,Wang, Zhenting.,Zhang, Caixia.,Geng, Xin.,...&Li, Danfeng.(2024).Physical weathering of Gobi Desert sediments under different temperature and humidity conditions.CATENA,234,12.
MLA Wang, Xunming,et al."Physical weathering of Gobi Desert sediments under different temperature and humidity conditions".CATENA 234(2024):12.

入库方式: OAI收割

来源:地理科学与资源研究所

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