Journal of Geographical Sciences ›› 2021, Vol. 31 ›› Issue (1): 3-45.doi: 10.1007/s11442-021-1831-2
• Review Article • Next Articles
CHEN Fahu1,2,3(), WU Shaohong3,4,5,*(
), CUI Peng2,3,6, CAI Yunlong7, ZHANG Yili2,3,4,5, YIN Yunhe4,5, LIU Guobin8, OUYANG Zhu3,4, MA Wei9, YANG Linsheng3,4,5, WU Duo10, LEI Jiaqiang11, ZHANG Guoyou4,12, ZOU Xueyong13, CHEN Xiaoqing2,6, TAN Minghong3,4,5, WANG Xunming3,4, BAO Anming11, CHENG Weixin4, DANG Xiaohu14, WEI Binggan4,5, WANG Guoliang8, WANG Wuyi4,5, ZHANG Xingquan4, LIU Xiaochen2,15, LI Shengyu11
Received:
2020-08-11
Accepted:
2020-10-08
Online:
2021-01-25
Published:
2021-03-25
Contact:
WU Shaohong
E-mail:fhchen@itpcas.ac.cn;wush@igsnrr.ac.cn
About author:
Chen Fahu, Academician of Chinese Academy of Sciences, E-mail: Supported by:
CHEN Fahu, WU Shaohong, CUI Peng, CAI Yunlong, ZHANG Yili, YIN Yunhe, LIU Guobin, OUYANG Zhu, MA Wei, YANG Linsheng, WU Duo, LEI Jiaqiang, ZHANG Guoyou, ZOU Xueyong, CHEN Xiaoqing, TAN Minghong, WANG Xunming, BAO Anming, CHENG Weixin, DANG Xiaohu, WEI Binggan, WANG Guoliang, WANG Wuyi, ZHANG Xingquan, LIU Xiaochen, LI Shengyu. Progress and prospects of applied research on physical geography and the living environment in China over the past 70 years (1949-2019)[J].Journal of Geographical Sciences, 2021, 31(1): 3-45.
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Figure 2
Schematic of the response of sand and sandstorms to human activities and changes in the Asian monsoon over the past 2000 years in the monsoon fringes of eastern China (after Chen et al., 2020). (a) The period of strong summer monsoon-strong human activity-desertification expansion-strong sandstorm; (b) The period of weak summer monsoon-weak human activity-vegetation restoration-weak sandstorm"
Figure 3
Comparison of saline-alkali soil and aeolian sandy soil before and after treatment in the Huang-Huai-Hai Plain; a and b show the results of wheat planting in the Beiqiuwa of Yucheng in the same year of heavy saline-alkali soil treatment using the shallow well group and strong drainage and irrigation technology (May 1990); c and d show the results of grape planting in Shahewa of Yucheng in the sandy land of an ancient river channel after treatment with the comprehensive aeolian sandy soil reversal technology (March 1989)."
Figure 5
Principle of the geographical detector (after Wang and Xu, 2017) The study area consists of two layers: the interpreted variable of Y and the spatial layer of X; X can be used to express geographical spatial stratified heterogeneity. $\bar{Y}$ and $\sigma^{2}$ are the mean and variance of the whole study area, $\bar{Y}_{h}$ and $\sigma^{2}_{h}$ are the mean and variance of the hth layer."
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