Impact of land use/cover change (LUCC) on sediment connectivity in small watersheds based on a revised index algorithm

被引:12
作者
Zhang, Qin [1 ,2 ]
Qin, Wei [1 ,2 ,4 ]
Ding, Lin [1 ,2 ]
Cao, Wenhong [1 ,2 ]
Xu, Haichao [1 ,2 ]
Liu, Qi [3 ]
Shi, Chenyu [1 ,2 ]
机构
[1] China Inst Water Resources & Hydropower Res, State Key Lab Simulat & Regulat Water Cycle River, Beijing 100048, Peoples R China
[2] Minist Water Resources, Res Ctr Soil & Water Conservat, Beijing 100048, Peoples R China
[3] Water Conservancy Comm Yellow River, Sci Trail Stn Soil & Water Conservat Tianshui City, Tianshui 741000, Peoples R China
[4] China Inst Water Resources & Hydropower Res, 20 Chegongzhuang West Rd, Beijing 100048, Peoples R China
基金
中国国家自然科学基金;
关键词
Sediment connectivity; Upslope confluence area; Land use/cover change; Sediment transport of watershed; Off-site impact; Loess Plateau; SOIL-EROSION; LANDSCAPE CONNECTIVITY; LOESS PLATEAU; RUNOFF; CATCHMENT; (DIS)CONNECTIVITY; YIELD; PATTERNS; DRIVEN; SPACE;
D O I
10.1016/j.geoderma.2023.116622
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Soil erosion is an important cause of global land degradation and other ecological and environmental problems. Revealing the influence mechanism of land use/cover change (LUCC) on sediment yield can provide a scientific basis for efficient comprehensive and decision-making management of watersheds. As an important indicator of sediment yield and transport capacity, sediment connectivity has been widely studied in recent years. However, the existing index of sediment connectivity (IC) ignores the influence of upslope land use/cover on confluence and the corresponding changes in downslope sediment transport. Moreover, a formula describing the upslope and downslope components does not establish an effective correlation with existing soil erosion formulas. Therefore, the index is not closely related to the erosion process and does not reflect the physical process of sediment transport and sediment deposition. In addition, there have been few reports concerning the effect of LUCC on sediment connectivity inside (on-site impact) and outside (off-site impact) the changed patches. Consequently, by based on addition of the revised parameters of the effective confluence area (Ar) and the runoff velocity factor (v) of the sediment delivery distributed (SEDD) model, an improved sediment connectivity index (ICZQ) is proposed. The results indicate that ICZQ has a significant linear relationship with annual runoff depth or sediment yield modulus in small watersheds within 100 km2 in the Loess Plateau, except for feature years containing rainstorm events (daily rainfall exceeding 50 mm). Therefore, the runoff and sediment transport capacity of small watersheds can be characterized by ICZQ under the influence of LUCC and rainfall change. In 1982-2020, driven by LUCC with an enhancement in vegetation (forest and grass), the ICZQ decreased in 90% of the area and decreased by a significant or extremely significant level over 48% of the area. To better understand the effects of LUCC on sediment connectivity, we analyzed on-site and off-site impacts with rainfall remaining unchanged to control the variables. The contribution rates of the on-site and off-site impacts caused by LUCC on sediment connectivity in Lvergou were 61% and 39%, 48% and 52%, respectively, over two typical periods (1985-1990 and 2015-2020). Due to the large proportion that off-site impacts occupied in the sediment connectivity change, the impact of LUCC on sediment connectivity cannot be ignored, especially when the associated scale is relatively small. The present study provides a quantitative method for the optimization of land use/cover patterns, such as vegetation restoration in watersheds along with a reference for further revealing the impact mechanism of erosion and sediment yield in watersheds.
引用
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页数:17
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