Effects of thawed depth on the sediment transport capacity by melt water on partially thawed black soil slope

2018 ◽  
Vol 30 (1) ◽  
pp. 84-93 ◽  
Author(s):  
Xiaofeng Gao ◽  
Fahu Li ◽  
Chao Chen ◽  
Yunyun Ban ◽  
Yuan Gao
Keyword(s):  
Sediment Transport ◽  
Black Soil ◽  
Soil Slope ◽  
Transport Capacity ◽  
Sediment Transport Capacity ◽  
Melt Water

scholarly journals Prediction of sediment transport capacity based on slope gradients and flow discharge

PLoS ONE ◽  
2021 ◽  
Vol 16 (9) ◽  
pp. e0256827
Author(s):  
Kai Zhang ◽  
Wang Xuan ◽  
Bai Yikui ◽  
Xu Xiuquan
Keyword(s):  
Sediment Transport ◽  
Overland Flow ◽  
Soil Slope ◽  
Transport Capacity ◽  
Slope Gradient ◽  
Particle Size Range ◽  
Flow Discharge ◽  
Brown Soil ◽  
Sediment Transport Capacity ◽  
Model Slope

Sediment transport capacity (Tc) is an essential parameter in the establishment of the slope soil erosion model. Slope type is an important crucial factor affecting sediment transport capacity of overland flow, and vegetation can effectively inhibit soil loss. Two new formulae of sediment transport capacity (Tc) are proposed of brown soil slope and vegetation slope in this study and evaluate the influence of slope gradient (S) and flow discharge (Q) on sediment transport capacity of different slope types. Laboratory experiments conducted using four flow discharges (0.35, 0.45, 0.55, and 0.65 L s-1), four slope gradients (3, 6, 9, and 12°), and two kinds of underlying surface (Brown soil slope, Vegetation slope). The soil particle size range is 0.05–0.5mm. The vegetation stems were 2mm in diameter and randomly arranged. The results show that the sediment transport capacity was positively correlated with the flow discharge and slope gradient. The vegetation slope’s average sediment transport capacity is 11.80% higher than the brown soil slope that same discharge and slope gradient conditions. The sensitivity of sediment transport capacity to flow discharge on brown soil slope is higher than that of slope gradient. The sensitivity of sediment transport capacity of vegetation slope to slope gradient is more heightened than flow discharge. The sediment transport capacity was well predicted by discharge and slope gradient on brown soil slope (R2 = 0.982) and vegetation slope (R2 = 0.993). This method is helpful to promote the study of the sediment transport process on overland flow.

Effect of stem basal cover on the sediment transport capacity of overland flows

Geoderma ◽  
2019 ◽  
Vol 337 ◽  
pp. 384-393 ◽  
Author(s):  
Hongli Mu ◽  
Xianju Yu ◽  
Suhua Fu ◽  
Bofu Yu ◽  
Yingna Liu ◽  
...  
Keyword(s):  
Sediment Transport ◽  
Transport Capacity ◽  
Basal Cover ◽  
Sediment Transport Capacity ◽  
Overland Flows

scholarly journals Effect of hydraulic parameters on sediment transport capacity in overland flow over erodible beds

2012 ◽  
Vol 16 (2) ◽  
pp. 591-601 ◽  
Author(s):  
M. Ali ◽  
G. Sterk ◽  
M. Seeger ◽  
M. Boersema ◽  
P. Peters
Keyword(s):  
Shear Stress ◽  
Sediment Transport ◽  
Hydraulic Parameters ◽  
Transport Capacity ◽  
Slope Gradient ◽  
Mean Flow ◽  
Stream Power ◽  
Unit Discharge ◽  
Sediment Transport Capacity ◽  
Mean Flow Velocity

Abstract. Sediment transport is an important component of the soil erosion process, which depends on several hydraulic parameters like unit discharge, mean flow velocity, and slope gradient. In most of the previous studies, the impact of these hydraulic parameters on transport capacity was studied for non-erodible bed conditions. Hence, this study aimed to examine the influence of unit discharge, mean flow velocity and slope gradient on sediment transport capacity for erodible beds and also to investigate the relationship between transport capacity and composite force predictors, i.e. shear stress, stream power, unit stream power and effective stream power. In order to accomplish the objectives, experiments were carried out in a 3.0 m long and 0.5 m wide flume using four well sorted sands (0.230, 0.536, 0.719, 1.022 mm). Unit discharges ranging from 0.07 to 2.07 × 10−3 m2 s−1 were simulated inside the flume at four slopes (5.2, 8.7, 13.2 and 17.6%) to analyze their impact on sediment transport rate. The sediment transport rate measured at the bottom end of the flume by taking water and sediment samples was considered equal to sediment transport capacity, because the selected flume length of 3.0 m was found sufficient to reach the transport capacity. The experimental result reveals that the slope gradient has a stronger impact on transport capacity than unit discharge and mean flow velocity due to the fact that the tangential component of gravity force increases with slope gradient. Our results show that unit stream power is an optimal composite force predictor for estimating transport capacity. Stream power and effective stream power can also be successfully related to the transport capacity, however the relations are strongly dependent on grain size. Shear stress showed poor performance, because part of shear stress is dissipated by bed irregularities, bed form evolution and sediment detachment. An empirical transport capacity equation was derived, which illustrates that transport capacity can be predicted from median grain size, total discharge and slope gradient.

A Simplified Equation for Modeling Sediment Transport Capacity

1989 ◽  
Vol 32 (5) ◽  
pp. 1545-1550 ◽  
Author(s):  
S. C. Finkner ◽  
M. A. Hearing ◽  
G. R. Foster ◽  
J. E. Gilley
Keyword(s):  
Sediment Transport ◽  
Transport Capacity ◽  
Sediment Transport Capacity

scholarly journals Sediment transport capacity of concentrated flows on steep loessial slope with erodible beds

2017 ◽  
Vol 7 (1) ◽  
Author(s):  
Hai Xiao ◽  
Gang Liu ◽  
Puling Liu ◽  
Fenli Zheng ◽  
Jiaqiong Zhang ◽  
...  
Keyword(s):  
Sediment Transport ◽  
Transport Capacity ◽  
Sediment Transport Capacity ◽  
Erodible Beds

Impacts of subsurface hydrologic conditions on rill sediment transport capacity

2020 ◽  
Vol 591 ◽  
pp. 125582
Author(s):  
Shuyuan Wang ◽  
Dennis C. Flanagan ◽  
Bernard A. Engel ◽  
Na Zhou
Keyword(s):  
Sediment Transport ◽  
Transport Capacity ◽  
Sediment Transport Capacity ◽  
Hydrologic Conditions
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