2020
DOI: 10.5846/stxb201909121903
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Changes in streamflow and sediment load in the catchments of the Loess Plateau, China: a review

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Cited by 2 publications
(4 citation statements)
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“…The conversion from cultivated land to forestland, scrub, or grassland (41,42,43) amounts to 5017.46 km 2 , with 3766.44 km 2 converted to grassland. Conversely, a total of 361.73 km 2 was converted from forestland, scrub, and grassland to cultivated land (14,24,34), indicating that there was a larger area of cultivated land being transformed into other types of land use compared with the opposite direction. Figure 3 illustrates the direction of the land-use type conversion across the basin in each landform type area.…”
Section: Analysis Of Land-use Change Tupu Process Between 1975 and 2015mentioning
confidence: 99%
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“…The conversion from cultivated land to forestland, scrub, or grassland (41,42,43) amounts to 5017.46 km 2 , with 3766.44 km 2 converted to grassland. Conversely, a total of 361.73 km 2 was converted from forestland, scrub, and grassland to cultivated land (14,24,34), indicating that there was a larger area of cultivated land being transformed into other types of land use compared with the opposite direction. Figure 3 illustrates the direction of the land-use type conversion across the basin in each landform type area.…”
Section: Analysis Of Land-use Change Tupu Process Between 1975 and 2015mentioning
confidence: 99%
“…From 1970 to the late 1990s, the government mainly carried out the comprehensive management of small watersheds and the construction of Three-North shelterbelts. After 2000, environmental governance focused on the projects of "Grain for Green" [14,15]. After years of environmental restoration, the overall vegetation cover area has increased, the sediment entering the Yellow River has reduced, and the land-use structure has also changed dramatically [13,[16][17][18][19].…”
Section: Introductionmentioning
confidence: 99%
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“…These measures have made considerable impacts and have reduced sediment exported from the LP to the Yellow River by 2.24 × 10 8 t year −1 in 1996, as compared to the sediment yield in 1970 [32]. The vegetation measures have increased total vegetation cover from 56% in 2000 to 76.8% in 2017 [33] and have been suggested as the main underlying surface factors affecting water and sediment changes in the LP [34]. Moreover, with the improvement in vegetation structure, the improvement in rainfall interception and soil infiltration by vegetation measures will become more and more significant [31], which will have a significant impact on the hydrological cycle of the LP area in the future.…”
Section: Introductionmentioning
confidence: 99%