Acta Geographica Sinica, Volume. 75, Issue 9, 1799(2020)
Fig. 1. Desertification area (a) and variability (b) in China from late 1950s to 2010 (according to Wang Tao et al. [113])
Fig. 2. A schematic diagram of the response of sandstorms to human activities and Asian monsoon changes in the eastern monsoon marginal region of China (according to Chen[130])
Fig. 3. Comparison of saline-alkali land and sandy land in the Huang-Huai-Hai Plain before and after treatment
Fig. 5. Principle of geodetector (according to Wang Jinfeng et al. [273]) (The study area consists of two layers: the explained variable
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Fahu CHEN, Shaohong WU, Peng CUI, Yunlong CAI, Yili ZHANG, Yunhe YIN, Guobin LIU, Zhu OUYANG, Wei MA, Linsheng YANG, Duo WU, Jiaqiang LEI, Guoyou ZHANG, Xueyong ZOU, Xiaoqing CHEN, Minghong TAN, Xunming WANG, Anming BAO, Weixin CHENG, Xiaohu DANG, Binggan WEI, Guoliang WANG, Wuyi WANG, Xingquan ZHANG, Xiaochen LIU, Shengyu LI.
Received: Mar. 3, 2020
Accepted: --
Published Online: Apr. 14, 2021
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