2017
DOI: 10.1080/20964129.2017.1401011
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Human settlement and changes in the distribution of river systems in the Minqin Basin over the past 2000 years in Northwest China

Abstract: Introduction: Arid area is an important base for human settlement, however, long and drastic human activities have altered the drainage patterns in the arid watersheds significantly, causing serious ecological consequences. This study, through a case study of the Minqin Basin, a microcosm of the artificial oases in the arid northwest China, used the multitypes of data to recover the spatial distribution of human settlement and drainage patterns during historical period and analyze the relationship between them… Show more

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Cited by 7 publications
(4 citation statements)
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“…Each set of characteristics has a corresponding range of habitability and population densities. In arid (desert) areas, people tend to live at oases or migrate upstream along the river network, driven by drought events exacerbated by severe evaporation and the drying out of downstream reaches (Ling et al, 2013; Xie et al, 2017). In the northeast plains, several water resources and fertile black soil provide suitable agricultural conditions, but the higher latitude and cold temperatures result in lower population density due to insufficient natural heat energy (Gao, 2012).…”
Section: Resultsmentioning
confidence: 99%
“…Each set of characteristics has a corresponding range of habitability and population densities. In arid (desert) areas, people tend to live at oases or migrate upstream along the river network, driven by drought events exacerbated by severe evaporation and the drying out of downstream reaches (Ling et al, 2013; Xie et al, 2017). In the northeast plains, several water resources and fertile black soil provide suitable agricultural conditions, but the higher latitude and cold temperatures result in lower population density due to insufficient natural heat energy (Gao, 2012).…”
Section: Resultsmentioning
confidence: 99%
“…OHR (102°50'0"-103°48'0" E, 38°26'45"-39°10'0" E), situated downstream from Shiyang River Basin (SRB) in northwestern China (Fig. 1), belongs to the cross belt of the Chinese Eastern Monsoon Region, Qinghai-Tibetan Alpine Region with dry climate [25]. The precipitation is about 115 mm per year and is mainly concentrated in July to September, while the potential evaporation is about 2,644 mm per year.…”
Section: Study Areamentioning
confidence: 99%
“…maxim, Peganum harmala, Artemisia arenaria, and Agriophyllum squarrosum are the native vegetation in this region [28]. Wetlands along rivers (or floodplain), were reclaimed for crop productions as early as Han Dynasty (2000 years ago) [29]. Currently, they are agricultural oases with high productivities and well-developed irrigation networks consisted of rivers, reservoirs, canals, and wells.…”
Section: Study Areamentioning
confidence: 99%