2021
DOI: 10.1029/2021gl095230
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Remote Sensing Characterization of Mountain Excavation and City Construction in Loess Plateau

Abstract: The population growth and urban expansion aggravate the tension between human and ecological environment, especially for the naturally fragile environments. The Loess Plateau in the vast mid-north China, including Shaanxi, Gansu, and Sichuan Provinces, covers an area of 624,641 km 2 (Wang, 2017). The loess is composed of million-year-old thick deposits of windblown dust and silt, which are subject to disaggregation under harsh climatic and soil conditions. The natural and anthropogenic deforestation has accele… Show more

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Cited by 21 publications
(5 citation statements)
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“…Regarding the research on dynamic environmental monitoring methods, remote sensing technology is often used in environmental monitoring, geological research, etc. Through remote sensing image technology, Hu et al conducted periodic geological monitoring [6]. Phiri et al applied satellite remote sensing data to monitor changes in land use and coverage based on summarizing remote sensing dynamic monitoring techniques [7].…”
Section: Introductionmentioning
confidence: 99%
“…Regarding the research on dynamic environmental monitoring methods, remote sensing technology is often used in environmental monitoring, geological research, etc. Through remote sensing image technology, Hu et al conducted periodic geological monitoring [6]. Phiri et al applied satellite remote sensing data to monitor changes in land use and coverage based on summarizing remote sensing dynamic monitoring techniques [7].…”
Section: Introductionmentioning
confidence: 99%
“…The exponential function model [11][12][13] assumes that the settlement rate decreases along the exponential curve with time. The model is expressed as follows:…”
Section: Exponential Function Modelmentioning
confidence: 99%
“…Because the hydraulic conductivity of aquitards is low, the response of aquitards lags behind the head change. Thus, we used an exponential decay model of time to characterize the evolution of the delayed subsidence [25,49]: b(t) = M e kt − 1 , where b(t) is the time series of displacement, M decreases the magnitude of the subsidence and k is the decay coefficient, which ranges from −1 to 0. A lower k indicates a greater decreasing trend of subsidence rate.…”
Section: Spatial and Temporal Variability Of Deformation In Xingtaimentioning
confidence: 99%