Threshold of watershed partition in SWAT based on separating hillslope and channel sediment simulations

Exploring how watershed partition influences hillslope and channel sediment in the Soil & Water Assessment Tool is important to identify the partition threshold and improve the model application in soil erosion evaluation. However, the influences on the channel phase, and the partition thres...

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Autores principales: Bingqing Lin, Dejian Zhang, Xingwei Chen, Huaxia Yao
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Lenguaje:EN
Publicado: Elsevier 2021
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spelling oai:doaj.org-article:362574b59ea745d79ec1c326cc4e6f772021-12-01T04:35:26ZThreshold of watershed partition in SWAT based on separating hillslope and channel sediment simulations1470-160X10.1016/j.ecolind.2020.107111https://doaj.org/article/362574b59ea745d79ec1c326cc4e6f772021-02-01T00:00:00Zhttp://www.sciencedirect.com/science/article/pii/S1470160X20310505https://doaj.org/toc/1470-160XExploring how watershed partition influences hillslope and channel sediment in the Soil & Water Assessment Tool is important to identify the partition threshold and improve the model application in soil erosion evaluation. However, the influences on the channel phase, and the partition threshold for the entire watershed sediment process have not yet been well addressed. The Xixi basin located in southeast China was taken as an example with thirteen partition levels. Based on the idea of separating the simulations of the hillslope and channel phases, the partition threshold for channel sediment routing was identified according to changes in the parameters of channel sediment routing and the spatial distributions of channel deposition under different partition levels with two newly proposed indicators. This allowed the partition threshold of the entire watershed sediment process to be determined by comparing the thresholds for channel and hillslope sediment. The results indicate that (1) watershed partition has a substantial influence on the spatial distributions of channel deposition, and increasing sub-watersheds decreases the spatial variations of channel deposition. However, the influences can be obscured at the watershed outlet by changing channel routing parameters. (2) The changes in channel sediment routing are primarily due to the sensitivity of the channel dimensions in the model to watershed partition, which alter the hydraulic radius until a partition threshold, at which point the mean sub-watershed size is 2.4% of the total watershed area. (3) The thresholds for hillslope sediment generation and channel sediment routing are different, and the threshold for effectively simulating the entire watershed sediment process mainly depend on the hillslope sediment phase with a mean sub-watershed size of approximately 1.6% of the total watershed area.Bingqing LinDejian ZhangXingwei ChenHuaxia YaoElsevierarticleChannel sediment routingPartition thresholdWatershed partitionSWATXixi basinEcologyQH540-549.5ENEcological Indicators, Vol 121, Iss , Pp 107111- (2021)
institution DOAJ
collection DOAJ
language EN
topic Channel sediment routing
Partition threshold
Watershed partition
SWAT
Xixi basin
Ecology
QH540-549.5
spellingShingle Channel sediment routing
Partition threshold
Watershed partition
SWAT
Xixi basin
Ecology
QH540-549.5
Bingqing Lin
Dejian Zhang
Xingwei Chen
Huaxia Yao
Threshold of watershed partition in SWAT based on separating hillslope and channel sediment simulations
description Exploring how watershed partition influences hillslope and channel sediment in the Soil & Water Assessment Tool is important to identify the partition threshold and improve the model application in soil erosion evaluation. However, the influences on the channel phase, and the partition threshold for the entire watershed sediment process have not yet been well addressed. The Xixi basin located in southeast China was taken as an example with thirteen partition levels. Based on the idea of separating the simulations of the hillslope and channel phases, the partition threshold for channel sediment routing was identified according to changes in the parameters of channel sediment routing and the spatial distributions of channel deposition under different partition levels with two newly proposed indicators. This allowed the partition threshold of the entire watershed sediment process to be determined by comparing the thresholds for channel and hillslope sediment. The results indicate that (1) watershed partition has a substantial influence on the spatial distributions of channel deposition, and increasing sub-watersheds decreases the spatial variations of channel deposition. However, the influences can be obscured at the watershed outlet by changing channel routing parameters. (2) The changes in channel sediment routing are primarily due to the sensitivity of the channel dimensions in the model to watershed partition, which alter the hydraulic radius until a partition threshold, at which point the mean sub-watershed size is 2.4% of the total watershed area. (3) The thresholds for hillslope sediment generation and channel sediment routing are different, and the threshold for effectively simulating the entire watershed sediment process mainly depend on the hillslope sediment phase with a mean sub-watershed size of approximately 1.6% of the total watershed area.
format article
author Bingqing Lin
Dejian Zhang
Xingwei Chen
Huaxia Yao
author_facet Bingqing Lin
Dejian Zhang
Xingwei Chen
Huaxia Yao
author_sort Bingqing Lin
title Threshold of watershed partition in SWAT based on separating hillslope and channel sediment simulations
title_short Threshold of watershed partition in SWAT based on separating hillslope and channel sediment simulations
title_full Threshold of watershed partition in SWAT based on separating hillslope and channel sediment simulations
title_fullStr Threshold of watershed partition in SWAT based on separating hillslope and channel sediment simulations
title_full_unstemmed Threshold of watershed partition in SWAT based on separating hillslope and channel sediment simulations
title_sort threshold of watershed partition in swat based on separating hillslope and channel sediment simulations
publisher Elsevier
publishDate 2021
url https://doaj.org/article/362574b59ea745d79ec1c326cc4e6f77
work_keys_str_mv AT bingqinglin thresholdofwatershedpartitioninswatbasedonseparatinghillslopeandchannelsedimentsimulations
AT dejianzhang thresholdofwatershedpartitioninswatbasedonseparatinghillslopeandchannelsedimentsimulations
AT xingweichen thresholdofwatershedpartitioninswatbasedonseparatinghillslopeandchannelsedimentsimulations
AT huaxiayao thresholdofwatershedpartitioninswatbasedonseparatinghillslopeandchannelsedimentsimulations
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