scholarly journals Characteristics of Surface Runoff for Four Vegetation Types in Small Watershed of Nver Zhai in West Hunan, China

2021 ◽  
Vol 50 (3) ◽  
pp. 603-611
Author(s):  
Jia Luo ◽  
Yongqiang Liu ◽  
Xuan Yi ◽  
Yuxin Tian ◽  
Xiaoling Zhou ◽  
...  
Keyword(s):  
Surface Runoff ◽  
Pinus Massoniana ◽  
Vegetation Types ◽  
Small Watershed ◽  
Mountain Area ◽  
Total Runoff ◽  
Significant Augmentation ◽  
Mixed Plantation ◽  
High Runoff ◽  
Sloping Farmland

Characteristics of the surface runoff of four vegetation types in the small watershed of Nver Zhai, Wuling Mountain Area, West Hunan were studied. Results indicated that, from June 10, 2015 to September 10, 2016 the precipitation recorded was up to 1971.80 mm, and there occurred 83 rainfalls during the period of investigation. With the increase in the rainfall, the surface runoff gradually increased, among which the Eucommia ulmoides Oliv. plantation showed significantly high runoff. When the rainfall gradually increased to 30 mm, the surface runoff was highest for the sloping farmland. Under an intense rainfall >50 mm, there was a significant augmentation in the surface runoff of the four types of forest lands, indicating that the soil water content began to reach to saturation. Furthermore, the total runoff of the different types of vegetation, the runoff depth and the runoff coefficient were in the order of: E. ulmoides plantation > Pinus massoniana Lamb. forest > Sloping farmland > maple- Cinnamomum camphora (L.) J. Presl. mixed plantation. Additionally, under the same rainfall, there was a reduction in the runoff with an increase in the evaporation, and the total runoff of maple- C. camphora mixed plantation was the lowest. Bangladesh J. Bot. 50(3): 603-611, 2021 (September)

scholarly journals Application of digital image processing in slope surface runoff velocity analysis under simulated rainfall conditions

2017 ◽  
Vol 49 (4) ◽  
pp. 1304-1312
Author(s):  
Tiexiong Gong ◽  
Yuanjun Zhu
Keyword(s):  
Image Processing ◽  
Surface Runoff ◽  
Lateral Diffusion ◽  
Ease Of Use ◽  
Velocity Analysis ◽  
Slope Gradient ◽  
Tracer Method ◽  
Dye Tracer ◽  
The Mean ◽  
High Runoff

Abstract To have accurate runoff velocity, there is need to improve dye tracer method for estimating surface runoff velocity. This can enhance the calculations of relevant hydrologic parameters that will lead to a better understanding of hydrological processes and soil erosion. In this study, an integrated dye tracer and image processing method (IPV) and dye tracer method (AOV), respectively, were used to estimate runoff velocity under three slope gradients (5°, 10°, and 15°) and three slope positions (up-slope, mid-slope, and down-slope). The results showed more variation in runoff velocity under IPV than AOV. Both IPV and AOV were positively correlated with slope gradient. IPV values were close to AOV ones for slope gradients ≤5°, but were significantly different for slope gradients ≥10°. The mean AOV value was 10.6% higher than that of IPV. Regression analysis showed that compared with AOV, IPV overestimated and underestimated runoff under low and high runoff velocity conditions, respectively. The use of image processing in IPV was advantageous because of its ease of use with fewer artificial errors and its suitability for lateral diffusion of runoff. Irrespectively, additional studies are needed to verify and/or improve further the use of this method in runoff velocity analysis.

scholarly journals Seasonal Surface Runoff Characteristics in the Semiarid Region of Western Heilongjiang Province in Northeast China—A Case of the Alun River Basin

Water ◽  
2019 ◽  
Vol 11 (3) ◽  
pp. 557
Author(s):  
Jinbai Huang ◽  
Kotaro Tagawa ◽  
Bin Wang ◽  
Jiawei Wen ◽  
Jingcai Wang
Keyword(s):  
River Basin ◽  
Surface Runoff ◽  
Peak Flow ◽  
Annual Runoff ◽  
Annual Rainfall ◽  
Semiarid Region ◽  
Heilongjiang Province ◽  
Runoff Coefficient ◽  
Total Runoff ◽  
Annual Means

Water resource issues are a challenging area of research in semiarid regions of the world. The objective of the current study was to reveal the main characteristics of seasonal surface runoff for the semiarid western Heilongjiang Province of China. The Alun River Basin, which has hydrological and meteorological characteristics of the local region, was adopted as the study location. A distributed rainfall-runoff combined with snowmelt hydrological model was used to carry out the runoff calculation for the six years (2011–2016). The results indicated that: The mean annual runoff coefficient was 0.34; snowmelt runoff accounted for 2.2% of annual total runoff in 2011–2016; the main part of annual rainfall and runoff was concentrated in the rainy season from June to September, the proportions of rainfall and runoff in this period were 78% and 86% to that of the annual means of 2011–2016; the peak flow represents a decreased trend since 2013, and evidently decreased in 2015 and 2016; less annual precipitation complex with paddy field retention of rainwater and runoff led to the peak flow and annual runoff coefficient in 2016 were obviously lower than that of annual means of 2011–2016. The results are expected to provide the basis for rational development and utilization of surface runoff, and further researches on surface runoff and water resources of the semiarid western Heilongjiang Province of China.

Evaluation of Sustainable Development of Typical Small Watershed in Mountain Area - A Case Study of Puwa Small Watershed

2011 ◽  
Vol 183-185 ◽  
pp. 729-733
Author(s):  
Cui Mei Ren ◽  
Wen Biao Duan ◽  
Ze Yu Li ◽  
Lin Meng ◽  
Li Yang
Keyword(s):  
Sustainable Development ◽  
Comprehensive Evaluation ◽  
Indicator System ◽  
Development Theory ◽  
Basic Operation ◽  
Small Watershed ◽  
Mountain Area ◽  
The Sustainable Development ◽  
Development Indicator ◽  
Pca Method

With rapid sponsorship and widely spreading of sustainable development theory, the research on the sustainable development indicator systems and its evaluation became increasingly an important issue for small watershed. Small watershed was thought to be the most basic operation unit for watershed sustainable development realization, building its sustainable development indicator system was regarded as the basic approach of realizing its sustainable development. Taking Puwa small watershed as study object, this paper quantitative analysis that the status of small watershed sustainable development by using AHP-PCA method. In this paper, taking AHP-PCA method as a powerful tool, by calculating comprehensive evaluation values of sustainable development as well as objective analysis of the level of sustainable development in different years the sustainable development situation of Puwa small watershed was evaluated. Corresponding strategies were put forward to supply relational decision-making departments with reference.

scholarly journals Impact of Arable Land to Grassland Conversion on the Vegetation-period Water Balance of a Small Agricultural Catchment (Němčický Stream)

2010 ◽  
Vol 5 (No. 4) ◽  
pp. 128-138 ◽  
Author(s):  
P. Kovář ◽  
D. Vaššová
Keyword(s):  
Land Use ◽  
Land Use Change ◽  
Water Balance ◽  
Surface Runoff ◽  
Arable Land ◽  
Vegetation Period ◽  
Water Balance Components ◽  
Total Runoff ◽  
Grassland Conversion ◽  
Pronounced Reduction

This paper presents results of decadal (10-day) water balance simulations for the vegetation periods (April to October) of 2001 (normal year), 2002 (wet year) and 2003 (dry year) in the Němčick&yacute; Stream experimental catchment (3.52 km<sup>2</sup>). The catchment is a typical agricultural area with a large extent of arable land. This paper shows that the model used (WBCM) is capable of reliably simulating decadal water balance components for the actual land use. The same model is then used to estimate water balance changes brought about when 10% of arable land has been transformed into permanent grassland. It is shown that this land use change results in a pronounced reduction of surface runoff and an increase in subsurface storage over the vegetation periods of all three years. The vegetation period groundwater runoff was only enhanced in the wet year, while the total runoff was reduced in all three years.&nbsp;

scholarly journals Impacts of Tile Drainage on Phosphorus Losses from Edge-of-Field Plots in the Lake Champlain Basin of New York

Water ◽  
2020 ◽  
Vol 12 (2) ◽  
pp. 328 ◽  
Author(s):  
Laura B. Klaiber ◽  
Stephen R. Kramer ◽  
Eric O. Young
Keyword(s):  
New York ◽  
Surface Runoff ◽  
Soluble Reactive Phosphorus ◽  
Tile Drainage ◽  
Total Runoff ◽  
Tile Drains ◽  
Reactive Phosphorus ◽  
Phosphorus Losses ◽  
Field Plots ◽  
Reduced Surface

Quantifying the influence of tile drainage on phosphorus (P) transport risk is important where eutrophication is a concern. The objective of this study was to compare P exports from tile-drained (TD) and undrained (UD) edge-of-field plots in northern New York. Four plots (46 by 23 m) were established with tile drainage and surface runoff collection during 2012–2013. Grass sod was terminated in fall 2013 and corn (Zea mays L.) for silage was grown in 2014 and 2015. Runoff, total phosphorus (TP), soluble reactive phosphorus (SRP), and total suspended solids (TSS) exports were measured from April 2014 through June 2015. Mean total runoff was 396% greater for TD, however, surface runoff for TD was reduced by 84% compared to UD. There was no difference in mean cumulative TP export, while SRP and TSS exports were 55% and 158% greater for UD, respectively. A three day rain/snowmelt event resulted in 61% and 84% of cumulative SRP exports for TD and UD, respectively, with over 100% greater TP, SRP and TSS exports for UD. Results indicate that tile drainage substantially reduced surface runoff, TSS and SRP exports while having no impact on TP exports, suggesting tile drains may not increase the overall P export risk.

Study on Four Different Vegetation Types Treating the Sanitary Sewage

2011 ◽  
Vol 105-107 ◽  
pp. 1985-1990
Author(s):  
Ming Tao Zhou ◽  
Ping Yang
Keyword(s):  
Water Quality ◽  
Surface Runoff ◽  
Festuca Arundinacea ◽  
Cynodon Dactylon ◽  
Vegetation Type ◽  
Vegetation Types ◽  
Total Removal ◽  
Artificial Surface ◽  
Quality Indexes ◽  
Better Than

The sanitary sewage is treated with four different vegetation types by means of artificial surface runoff. Results show soil+ Cynodon dactylon L. + Festuca arundinacea Schreb is the best vegetation type in treating the sanitary sewage, and the total removal of it is 80.24% TN, 62.99% TP, 74.85% BOD5, 39.73% COD and 58.64% TOC respectively in the course of trial, which indicates that the mixed vegetation type made up of plants and soil is better than the pure soil vegetation type, and the complementary collocation of complex plants is better than the single plant.Five water-quality indexes of the sanitary sewage removed by the single vegetation type are also studied, and it shows that there are some differences among them from high to low as follows: TN>BOD5>TP>TOC>COD.

scholarly journals Freshwater flux to Sermilik Fjord, SE Greenland

2010 ◽  
Vol 4 (3) ◽  
pp. 1195-1224 ◽  
Author(s):  
S. H. Mernild ◽  
G. E. Liston ◽  
I. M. Howat ◽  
Y. Ahn ◽  
K. Steffen ◽  
...  
Keyword(s):  
Surface Runoff ◽  
Meteorological Data ◽  
Greenland Ice Sheet ◽  
Freshwater Flux ◽  
Terrestrial Runoff ◽  
Ice Melt ◽  
Total Runoff ◽  
Glacier Terminus ◽  
Frictional Melting ◽  
Catchment Runoff

Abstract. Fluctuations in terrestrial surface freshwater flux to Sermilik Fjord, SE Greenland, were simulated and analyzed. SnowModel, a state-of-the-art snow-evolution, snow and ice melt, and runoff modeling system, was used to simulate the temporal and spatial terrestrial runoff distribution to the fjord based on observed meteorological data (1999–2008) from stations located on and around the Greenland Ice Sheet (GrIS). Simulated runoff was compared and verified against independent glacier catchment runoff observations (1999–2005). Modeled runoff to Sermilik Fjord was highly variable, ranging from 2.9×109 m3 y−1 in 1999 to 5.9×109 m3 y−1 in 2005. The uneven spatial runoff distribution produced an areally-averaged annual maximum runoff at the Helheim glacier terminus of more than 3.8 m w.eq. The sub-catchment runoff of the Helheim glacier region accounted for 25% of the total runoff to Sermilik Fjord. The runoff distribution from the different sub-catchments suggested a strong influence from the spatial variation in glacier coverage. To assess the Sermilik Fjord freshwater flux, simulated terrestrial runoff and net precipitation (precipitation minus evaporation and sublimation) for the fjord area were combined with satellite-derived ice discharge and subglacial geothermal and frictional melting due to basal ice motion. A terrestrial freshwater flux of ~40.4×109 m3 y−1 was found for Sermilik Fjord, with an 11% contribution originated from surface runoff. For the Helheim glacier sub-catchment only 4% of the flux originated from terrestrial surface runoff.

scholarly journals Quantitative Assessment of Surface Runoff and Base Flow Response to Multiple Factors in Pengchongjian Small Watershed

Forests ◽  
2018 ◽  
Vol 9 (9) ◽  
pp. 553 ◽  
Author(s):  
Lei Ouyang ◽  
Shiyu Liu ◽  
Jingping Ye ◽  
Zheng Liu ◽  
Fei Sheng ◽  
...  
Keyword(s):  
Surface Runoff ◽  
Climatic Factors ◽  
Dynamic Change ◽  
Vegetation Restoration ◽  
Base Flow ◽  
Small Watershed ◽  
Runoff Generation ◽  
Multiple Factors ◽  
Precipitation Variation ◽  
Annual Scale

Quantifying the impacts of multiple factors on surface runoff and base flow is essential for understanding the mechanism of hydrological response and local water resources management as well as preventing floods and droughts. Despite previous studies on quantitative impacts of multiple factors on runoff, there is still a need for assessment of the influence of these factors on both surface runoff and base flow in different temporal scales at the watershed level. The main objective of this paper was to quantify the influence of precipitation variation, evapotranspiration (ET) and vegetation restoration on surface runoff and base flow using empirical statistics and slope change ratio of cumulative quantities (SCRCQ) methods in Pengchongjian small watershed (116°25′48″–116°27′7″ E, 29°31′44″–29°32′56″ N, 2.9 km2), China. The results indicated that, the contribution rates of precipitation variation, ET and vegetation restoration to surface runoff were 42.1%, 28.5%, 29.4% in spring; 45.0%, 37.1%, 17.9% in summer; 30.1%, 29.4%, 40.5% in autumn; 16.7%, 35.1%, 48.2% in winter; and 35.0%, 38.7%, 26.3% in annual scale, respectively. For base flow they were 33.1%, 41.9%, 25.0% in spring; 39.3%, 51.9%, 8.8% in summer; 40.2%, 38.2%, 21.6% in autumn; 24.3%, 39.4%, 36.3% in winter; and 24.4%, 47.9%, 27.7% in annual scale, respectively. Overall, climatic factors, including precipitation and ET change, affect surface runoff generation the most, while ET affects the dynamic change of annual base flowthe most. This study highlights the importance of optimizing forest management to protect the water resource.

scholarly journals Effects of rainfall intensity on runoff and nutrient loss of gently sloping farmland in a karst area of SW China

PLoS ONE ◽  
2021 ◽  
Vol 16 (3) ◽  
pp. e0246505
Author(s):  
Yiwen Yao ◽  
Quanhou Dai ◽  
Ruxue Gao ◽  
Yixian Gan ◽  
Xingsong Yi
Keyword(s):  
Surface Runoff ◽  
Rainfall Intensity ◽  
Simulation Method ◽  
Nutrient Loss ◽  
Rainfall Simulation ◽  
Karst Area ◽  
Nutrient Losses ◽  
Nutrient Runoff ◽  
Karst Areas ◽  
Sloping Farmland

Nutrient losses from sloping farmland in karst areas lead to the decline in land productivity and nonpoint source pollution. A specially tailored steel channel with an adjustable slope and underground hole fissures was used to simulate the microenvironment of the "dual structure" of the surface and underground of sloping farmland in a karst area. The artificial rainfall simulation method was used to explore the surface and underground runoff characteristics and nutrient losses from sloping farmland under different rainfall intensities. The effect of rainfall intensity on the nutrient loss of farmland on karst sloping land was clarified. The results showed that the surface was the main route of runoff and nutrient loss during the rainy season on sloping farmland in karst areas. The influence of rainfall intensity on the nutrients in surface runoff was more substantial than that on underground runoff nutrients. Nutrient loss was more likely to occur underground than on the surface. The losses of total nitrogen, total phosphorus, and total potassium in surface and underground runoff initially increased and then gradually stabilized with the extension of rainfall duration and increased with increasing rainfall intensity and the amount of nutrient runoff. The output of nutrients through surface runoff accounted for a high proportion of the total, and underground runoff was responsible for a low proportion. Although the amount of nutrients output by underground runoff was small, it could directly cause groundwater pollution. The research results provide a theoretical reference for controlling land source pollution from sloping farming in karst areas.

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