水保所知识产出(1956---)知识库

Ephemeral gullies (EGs) play a crucial role in hydrological connectivity, soil erosion,
and land degradation. However, little research has focused on flow hydraulics in con-
centrated flow channels and their effects on EG erosion on steep loessial slopes. A
simulated experiment of rainfall (60–120 mm hr ?1 ) and upslope inflow (0.45–
2.25 m 2 hr ?1 ) were conducted on concentrated flow channels with loess at 15 ? –25 ?
slope gradients. The concentrated flow was turbulent and subcritical in most cases.
The flow shear stress, stream power, and unit stream power in the concentrated flow
channels varied from 32.65 to 109.40 N m ?2 , 10.85 to 38.66 N m ?1 s ?1 , and 0.08 to
0.16 m s ?1 , respectively. The EG depth, width, and width-depth ratio varied within
14.8–24.6 cm, 18.5–33.8 cm, and 1.13–1.83, respectively. Moreover, the EG depth
and width increased in a power function with the runoff rate (R 2 = 0.82–0.83;
p < 0.01). The sediment yield rate (Ys) varied within 15.94–94.44 g m ?2 s ?1 under
the different treatments and had a good linear relationship with the runoff rate
(R 2 = 0.78; p < 0.01). Furthermore, the flow shear stress and stream power can be
used to predict Ys by linear functions. The critical runoff rate and shear stress to initi-
ate EG erosion were determined to be 0.09 m 3 hr ?1 and 2.66 N m ?2 . However, the
coefficient of determination for the linear relationship between Ys and shear stress
was low (0.58). The results indicate that the flow shear stress mechanism might not
be enough to explain sediment load variation for EG erosion, and headcut erosion
mechanism should be taken into account.