Trends in River Total Suspended Sediments Driven by Dams and Soil Erosion: A Comparison Between the Yangtze and Mekong Rivers
Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt
Standard
Trends in River Total Suspended Sediments Driven by Dams and Soil Erosion : A Comparison Between the Yangtze and Mekong Rivers. / Guan, Qi; Feng, Lian; Tang, Jing; Park, Edward; Ali, Tarig A.; Zheng, Yi.
I: Water Resources Research, Bind 58, Nr. 10, e2022WR031979, 2022.Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt
Harvard
APA
Vancouver
Author
Bibtex
}
RIS
TY - JOUR
T1 - Trends in River Total Suspended Sediments Driven by Dams and Soil Erosion
T2 - A Comparison Between the Yangtze and Mekong Rivers
AU - Guan, Qi
AU - Feng, Lian
AU - Tang, Jing
AU - Park, Edward
AU - Ali, Tarig A.
AU - Zheng, Yi
PY - 2022
Y1 - 2022
N2 - Global river systems are experiencing rapid changes in sediment transport under growing anthropogenic and climatic stresses. However, the response of sediment discharge to the coupled influence of anthropogenic and natural factors and the associated impacts on the fluvial geomorphology in the Yangtze and Mekong rivers are not comprehensively assessed. Here, we recalibrated a seamless retrieval algorithm of the total suspended sediment (TSS) concentrations using in situ data and concurrent satellite data sets to analyze spatiotemporal patterns of the TSS concentrations in the lower Yangtze and Mekong rivers. Combined with soil erosion rates estimated by the Revised Universal Soil Loss Equation for the past 20 years, we examined the contributions of different factors to TSS trends. The results show that TSS concentrations in the Yangtze River decreased from 0.47 g L-1 in 2000 to 0.23 g L-1 in 2018 due to the construction of the Three Gorges Dam (TGD), especially in the Jingjiang reach, with a declining magnitude of 0.3 g L-1 (similar to 56%) since the TGD began operating. The Mekong River experienced increasing TSS concentration trends upstream and decreasing trends downstream from 2000 to 2018, possibly attributed to increased upstream soil erosion and decreased downstream water discharge. Declining TSS concentrations in both rivers have driven varying degrees of river channel erosion over the past two decades. This study investigated long-term changes in the TSS concentrations and soil erosion in the Yangtze and Mekong rivers, and the results provide baseline information for the sustainable development of river sediment delivery.
AB - Global river systems are experiencing rapid changes in sediment transport under growing anthropogenic and climatic stresses. However, the response of sediment discharge to the coupled influence of anthropogenic and natural factors and the associated impacts on the fluvial geomorphology in the Yangtze and Mekong rivers are not comprehensively assessed. Here, we recalibrated a seamless retrieval algorithm of the total suspended sediment (TSS) concentrations using in situ data and concurrent satellite data sets to analyze spatiotemporal patterns of the TSS concentrations in the lower Yangtze and Mekong rivers. Combined with soil erosion rates estimated by the Revised Universal Soil Loss Equation for the past 20 years, we examined the contributions of different factors to TSS trends. The results show that TSS concentrations in the Yangtze River decreased from 0.47 g L-1 in 2000 to 0.23 g L-1 in 2018 due to the construction of the Three Gorges Dam (TGD), especially in the Jingjiang reach, with a declining magnitude of 0.3 g L-1 (similar to 56%) since the TGD began operating. The Mekong River experienced increasing TSS concentration trends upstream and decreasing trends downstream from 2000 to 2018, possibly attributed to increased upstream soil erosion and decreased downstream water discharge. Declining TSS concentrations in both rivers have driven varying degrees of river channel erosion over the past two decades. This study investigated long-term changes in the TSS concentrations and soil erosion in the Yangtze and Mekong rivers, and the results provide baseline information for the sustainable development of river sediment delivery.
KW - total suspended sediment
KW - dam
KW - MODIS
KW - Yangtze
KW - Mekong
KW - soil erosion
KW - 3 GORGES DAM
KW - LAND-USE
KW - COASTAL WATERS
KW - BASIN
KW - CHANGJIANG
KW - DISCHARGE
KW - IMPACTS
KW - SEA
KW - VARIABILITY
KW - HYDROPOWER
U2 - 10.1029/2022WR031979
DO - 10.1029/2022WR031979
M3 - Journal article
VL - 58
JO - Water Resources Research
JF - Water Resources Research
SN - 0043-1397
IS - 10
M1 - e2022WR031979
ER -
ID: 322875154