Characteristics of surface flow and interflow and nitrogen loss in Quercus acutissima forest land under simulated rainfall

2019 ◽  
Vol 39 (8) ◽  
Author(s):  
王荣嘉 WANG Rongjia ◽  
高鹏 GAO Peng ◽  
李成 LI Cheng ◽  
刘潘伟 LIU Panwei ◽  
孙鉴妮 SUN Jianni ◽  
...  
CATENA ◽  
2016 ◽  
Vol 139 ◽  
pp. 73-81 ◽  
Author(s):  
Weimin Xing ◽  
Peiling Yang ◽  
Shumei Ren ◽  
Chang Ao ◽  
Xu Li ◽  
...  

2019 ◽  
Vol 16 (5) ◽  
pp. 1048-1064 ◽  
Author(s):  
Long-zhou Deng ◽  
Kai Fei ◽  
Tian-yu Sun ◽  
Li-ping Zhang ◽  
Xiao-juan Fan ◽  
...  

2020 ◽  
Vol 12 (3) ◽  
pp. 1146 ◽  
Author(s):  
Nan Zhang ◽  
Qun Zhang ◽  
Yueqiao Li ◽  
Mansheng Zeng ◽  
Wan Li ◽  
...  

Periods of consecutive days with heavy rain of high intensity are common in the red soil region of China, increasing unpredictable risks of soil erosion and non-point source pollution on sloping orchards. Grass cover, as a type of vegetation management, is useful for controlling soil erosion and pollution. However, the potential of different kinds of groundcover plants in combating soil erosion and non-point source pollution remains unclear under the rainfall conditions in this region of China. This study included 7 d of simulated rainfall applied to a set of six treatments: Bare soil control, natural grass, and four groundcover treatments, Trifolium repens, T. repens, and Lolium perenne, Vicia sativa and Festuca elata, Medicago polymorpha, and Cynodon dactylon. The effects of the treatments on runoff volume, and soil, nitrogen, and phosphorus losses were evaluated. The results indicated that greater soil erosion and non-point source pollution occurred over the first 3d of daily 1-h simulated rainfall events. Also, the beneficial effects of the groundcover plants were greater earlier in the 7-d period of daily heavy rain, particularly in reducing runoff and nitrogen loss on the second and third day. Compared with bare soil, all the groundcovers showed a reduction effect in varying degrees, among which T. repens treatment was more effective. T. repens treatment showed an overall reduction in runoff and soil loss by 25.5% and 91.5%, respectively, and total nitrogen, nitrate nitrogen, ammonia nitrogen and total phosphorus loss by 25.5%, 74.6%, 90.7%, and 81.8%, respectively. These findings indicated that single planting of perennial pasture T. repens with short stems is an effective management option to limit soil erosion and non-point source pollution in sloping citrus orchards of southern China.


2020 ◽  
Vol 591 ◽  
pp. 125318 ◽  
Author(s):  
Yuanyuan Li ◽  
Gary Feng ◽  
Haile Tewolde ◽  
Mingyi Yang ◽  
Fengbao Zhang

2017 ◽  
Vol 7 (23) ◽  
pp. 10131-10142 ◽  
Author(s):  
Xianwei Song ◽  
Yang Gao ◽  
Sophie M. Green ◽  
Jennifer A. J. Dungait ◽  
Tao Peng ◽  
...  

2020 ◽  
Author(s):  
Tian Wang ◽  
Zhilin Huang ◽  
Liang Ma ◽  
Lixiong Zeng

<p>Rainfall intensity and duration directly affect the process of soil nutrient loss. In this paper, long-term, low-intensity rainfall (LL) (58.4mm rainfall, 605min duration) and short-term, high-intensity rainfall (SH) (59.2mm rainfall, 287min duration) were selected to study the pathway for soil nitrogen and phosphorus loss and load differentiation under different rainfall modes by using a slope experiment plot. The results indicated that: (1) The difference between the runoff duration of LL (3410min) and that of SH (410min) was obvious, and the runoff rate was 14.44% and 28.55%, respectively; (2) There were different nutrient concentration distributions. On one hand, the concentration of TN in the surface flow was lower than that in the interflow. The average TN concentration in the surface flow of LL and SH was 13.7 and 16.94 mg·L<sup>-1</sup>, respectively. The average TN concentration in the interflow of LL and SH was 59.25 and 50.89 mg·L<sup>-1</sup>, respectively. On the other hand, the concentration of TP in the surface flow was higher than that in the interflow. The concentration of TP ranged from 0.42 to 1.44 mg·L<sup>-1</sup> in the surface flow, and from 0.21 to 0.91 mg·L<sup>-1</sup> in the interflow; (3) The interflow is the main pathway of nitrogen loss, while the surface flow is the main pathway of phosphorus loss. The respective TN load of LL and SH runoff was 4.04 and 8.49 kg·hm<sup>-2</sup>, of which the contribution rate of the interflow was 88.49% and 85.54%, respectively. Additionally, the respective TP load of LL and SH runoff was 0.11 and 0.33 kg·hm<sup>-2</sup>, of which the contribution rate of the surface flow was 65.79% and 70.67%, respectively; (4) The amount of rainfall was almost the same but its intensity was different. High intensity rainfall would cause greater soil nutrient loss. The amount of total nitrogen and phosphorus loss in a sloppy land due to SH rainfall was 2-3 times higher than that due to LL rainfall.</p>


Soil Research ◽  
1990 ◽  
Vol 28 (4) ◽  
pp. 641 ◽  
Author(s):  
RG Palis ◽  
G Okwach ◽  
CW Rose ◽  
PG Saffigna

Thirty-five erosion experiments, involving four levels of surface contact cover by corn stalks and corn leaves (the latter represented by flat metal sheets) on three slopes, were carried out under simulated rainfall to investigate the effect of fractional surface contact cover and type on the loss and enrichment ratio (ER) of nitrogen in eroded sediment. All experiments were in a tilting flume of the simulated rainfall facility with a sandy clay loam soil. Experiments with rainfall detachment as the only erosion process were conducted on a low slope of 0.1%, to prevent entrainment occurring. The simulated rainfall rate was 100 mm h-1, and sediment samples were collected at the flume exit for up to 40 min. In experiments with entrainment as the only erosion process, clear water was applied as runon at the top of the flume. A stream power of 0 33 W m-2 was used and maintained with entrainment alone and in experiments with rainfall and runon combined for both 3 and 6% slopes. Sediment samples were fractionated through a series of sieves and total nitrogen was analysed for each size range to give the enrichment ratio (ER). The aggregate size or settling velocity characteristics, enrichment ratio (ER), and total nitrogen loss of the eroded sediment varied considerably with slope and cover types for the different erosion experiments. As cover by corn stalks increased, the settling velocity characteristics of eroded sediment became finer; the degree of this fineness was greater than when simulated leaves provided the same cover. For the rainfall detachment alone experiments, values of ER were greater than unity for both cover types and slopes, and greater than values for all other experiments. For the combined rainfall and runon experiments, ER was higher for corn stalks than simulated leaves. For experiments with entrainment alone, values of ER were close to unity for both cover types and slope, even by the early sampling time of 0.6 min. It may be concluded that the effectiveness of cover in reducing nutrient loss lies in reducing sediment loss, not in reducing ER. When rainfall detachment and entrainment were applied together, sediment concentration and total nitrogen loss were substantially increased over the sum of the contribution of rainfall detachment and entrainment acting alone. This finding indicates synergism in nutrient loss between these two erosion processes.


Sign in / Sign up

Export Citation Format

Share Document