2017
DOI: 10.3390/w9090687
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Virtual Water Flows at the County Level in the Heihe River Basin, China

Abstract: Water scarcity in arid regions can be addressed by using the virtual water concept in water resources management. This research used a compiled county-level input-output table to analyze virtual water flows for the Heihe River Basin in 2012 by applying a multi-regional input-output (MRIO) model. The results showed that the Heihe River Basin is a net virtual water exporter at a scale of 1.05 billion m 3 , which accounts for one third of the total amount of the basin's water resources. The midstream area of the … Show more

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Cited by 10 publications
(3 citation statements)
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“…It can decompose to obtain the internal drivers that lead to changes in VW flows, thus exploring the trade causes of water scarcity in greater depth. Even so, the application of SDA models could be improved: first, SDA is usually applied at the interprovincial level and lacks analysis at the national level [36][37][38][39][40]. Although Cai et al (2019) used SDA to assess drivers of VW flows in China, only the 2002, 2007, and 2012 years were analyzed due to data availability [17].…”
Section: Introductionmentioning
confidence: 99%
“…It can decompose to obtain the internal drivers that lead to changes in VW flows, thus exploring the trade causes of water scarcity in greater depth. Even so, the application of SDA models could be improved: first, SDA is usually applied at the interprovincial level and lacks analysis at the national level [36][37][38][39][40]. Although Cai et al (2019) used SDA to assess drivers of VW flows in China, only the 2002, 2007, and 2012 years were analyzed due to data availability [17].…”
Section: Introductionmentioning
confidence: 99%
“…In the water cycle, the hydrogen and oxygen isotopic compositions of various water bodies are affected by isotopic fractionation, which has wide spatial and temporal heterogeneity. Water bodies from different sources have different isotopic characteristics (Zhang et al 2006, Zhang et al 2007). The utility of δ 18 O and δ 2 H values depends on the sources and seasonal changes in different hydrological intervals as follows: due to the low temperatures and reduced evaporation, heavy isotope levels are lower in winter snow than in summer rain; compared with that of source water, the heavy isotope content of surface water bodies experiencing evaporation is higher; and longer water transport time usually leads to lower variance and seasonal amplitude of stable isotopes in runoff and groundwater compared with seasonal precipitation (McGuire et al 2006, Soulsby et al 2015, Vystavna et al 2017).…”
Section: Introductionmentioning
confidence: 99%
“…Some researchers studied the water footprint and virtual water trade in China (or other countries) or a specific province with the single-region input-output model [17][18][19][20][21][22][23][24]. Many researchers studied the water footprint and virtual water trade in multiple regions or provinces of China (or other countries) with the multi-region input-output model [25][26][27][28][29][30][31][32][33][34].…”
Section: Introductionmentioning
confidence: 99%