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  • 1
    In: Chest, Elsevier BV, Vol. 161, No. 4 ( 2022-04), p. 960-970
    Type of Medium: Online Resource
    ISSN: 0012-3692
    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2022
    detail.hit.zdb_id: 2007244-2
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  • 2
    In: Water Supply, IWA Publishing, Vol. 18, No. 6 ( 2018-12-01), p. 2142-2150
    Abstract: Overland flow is influenced by the spatial variability of the watershed surface and the distribution of vegetation in the process of confluence. Thus, Manning's roughness coefficient, in different directions on the slope, has different values. This causes different effects on the resistance to flow in the downstream direction of each grid cell, affecting the flow distribution among the grid cells of a distributed hydrological model. To show that the spatial variation of the overland vegetation had the effect of directional difference resistance to the overland flow, this study used an indoor fixed-bed test. We used a cylinder to simulate the stems of the vegetation used in the study. We modeled the relationship between Manning's roughness coefficient and flow depth and studied this relationship for three types of vegetation distributed at three different slopes of 0.0%, 0.5%, and 1.0%. The slopes were based on three angles of 30°, 45°, and 90° between the vegetation rows and flow. The results showed that the resistance of overland flow had directional differences caused by the spatial variability of the vegetation distribution. At the same slope and flow depth, Manning's roughness coefficient decreased as the angle between flow and vegetation rows increased. At the same slope, the angle between flow and vegetation rows and Manning's roughness coefficient increased as flow depth increased. The slope did not affect the law of Manning's roughness coefficient with changes in the angle between flow and vegetation rows.
    Type of Medium: Online Resource
    ISSN: 1606-9749 , 1607-0798
    RVK:
    Language: English
    Publisher: IWA Publishing
    Publication Date: 2018
    detail.hit.zdb_id: 2967640-X
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  • 3
    Online Resource
    Online Resource
    Korean Society of Environmental Engineering ; 2016
    In:  Environmental Engineering Research Vol. 21, No. 3 ( 2016-09-30), p. 226-232
    In: Environmental Engineering Research, Korean Society of Environmental Engineering, Vol. 21, No. 3 ( 2016-09-30), p. 226-232
    Type of Medium: Online Resource
    ISSN: 1226-1025
    Language: English
    Publisher: Korean Society of Environmental Engineering
    Publication Date: 2016
    detail.hit.zdb_id: 2976690-4
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  • 4
    Online Resource
    Online Resource
    Springer Science and Business Media LLC ; 2018
    In:  Iranian Journal of Science and Technology, Transactions of Civil Engineering Vol. 42, No. 4 ( 2018-12), p. 381-390
    In: Iranian Journal of Science and Technology, Transactions of Civil Engineering, Springer Science and Business Media LLC, Vol. 42, No. 4 ( 2018-12), p. 381-390
    Type of Medium: Online Resource
    ISSN: 2228-6160 , 2364-1843
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2018
    detail.hit.zdb_id: 2843076-1
    SSG: 11
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  • 5
    Online Resource
    Online Resource
    IWA Publishing ; 2018
    In:  Water Science and Technology Vol. 78, No. 11 ( 2018-12-28), p. 2383-2391
    In: Water Science and Technology, IWA Publishing, Vol. 78, No. 11 ( 2018-12-28), p. 2383-2391
    Abstract: Vegetation is an important part of the natural environment and has resistance effects on overland runoff, which can effectively reduce hydraulic erosion. The effect of vegetation stem diameter and slope gradient on flow resistance is thus worthy of further study. The influence of three different slope gradients (s), three vegetation stem diameters (d) and 12 levels of unit discharge (q) on the flow resistance of a slope was simulated to systematically study the effect of vegetation stem diameter and slope gradient on overland runoff. The diameter of the vegetation stem and the slope gradient were found to have a significant resistance effect on overland runoff. Under the same slope gradient, the Darcy–Weisbach resistance factor (f) increased with an increase in the vegetation stem diameter. Under experimental conditions, the rate of change of f was analysed by linear regression, and as d increased by 1 mm, f increased by an average of 49.9%. For a given vegetation stem diameter and vegetation distribution pattern, the greater the slope gradient, the smaller the value of f, and as S increased by 1.0%, f decreased by an average of 24.5%. These results are important to optimize the slope vegetation distribution in farmland conservation.
    Type of Medium: Online Resource
    ISSN: 0273-1223 , 1996-9732
    Language: English
    Publisher: IWA Publishing
    Publication Date: 2018
    detail.hit.zdb_id: 764273-8
    detail.hit.zdb_id: 2024780-1
    SSG: 14
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  • 6
    Online Resource
    Online Resource
    IWA Publishing ; 2017
    In:  Water Supply Vol. 17, No. 1 ( 2017-02-01), p. 24-31
    In: Water Supply, IWA Publishing, Vol. 17, No. 1 ( 2017-02-01), p. 24-31
    Abstract: The presence of orderly arranged rows and spacing of crop vegetation increases the anisotropy of the Earth's surface, and affects the resistance of the surface to overland flow. However, few studies have addressed how the orderly arrangement of crop vegetation affects the resistance of the surface to overland flow. In the present study, we consider that flow resistance has anisotropic attributes. We have also performed a flow resistance experiment using rigid and simulated partially submerged crop vegetation. The simulation replicated water flow in different directions over the same crop vegetation and overland surface. The angles of flow direction and the crop rows were arranged as 15 °, 30 °, 45 °, and 90 °. The results show that the flow resistance of partially submerged crop vegetation is composed of surface resistance ns and vegetation resistance np. Vegetation resistance np is linearly proportional to the submerged vegetation height h, and the proportionality coefficient α (Δn/Δh) varies with the angle θ of the flow direction and the crop rows under the same water depth conditions, n15 & gt; n30 & gt; n45 & gt; n90. Further regression analysis revealed that the relationship between the coefficient α and vertical projection width of crop stems in the flow direction is a power function.
    Type of Medium: Online Resource
    ISSN: 1606-9749 , 1607-0798
    RVK:
    Language: English
    Publisher: IWA Publishing
    Publication Date: 2017
    detail.hit.zdb_id: 2967640-X
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  • 7
    Online Resource
    Online Resource
    IWA Publishing ; 2018
    In:  Hydrology Research Vol. 49, No. 6 ( 2018-12-01), p. 1991-2001
    In: Hydrology Research, IWA Publishing, Vol. 49, No. 6 ( 2018-12-01), p. 1991-2001
    Abstract: Soil erosion of farmland is a major issue faced by the agricultural industry. Control of water-induced erosion can be improved through the simulation of different configurations of vegetation row direction to analyze the effects of farmland vegetation row directions RD on the hydraulic characteristics of flow. The farmland vegetation row directions were simulated and the anisotropic influence of the farmland vegetation row direction on flow hydraulic characteristics was experimentally analyzed. Three groups of farmland vegetation row directions with angles θ of 15°, 45°, and 90° with respect to the flow direction FD were configured. Experimental results show that different angles caused variation in hydraulic parameters velocity V, Reynolds number Re, Froude number Fr, and Darcy–Weisbach friction factor λ along the directions of flow. The rates of change of λ, Re, and Fr were analyzed statistically, where θ was increased every 10°; the average rate of decrease of λ was 5.2% and the average rates of increase of Re and Fr were 2.2% and 3.4%, respectively. These results indicate that the vegetation distribution pattern on farmland has an anisotropic influence on the hydraulic characteristics of flow. This investigation provides valuable references for the optimization of farmland vegetation distribution and soil erosion control.
    Type of Medium: Online Resource
    ISSN: 0029-1277 , 2224-7955
    Language: English
    Publisher: IWA Publishing
    Publication Date: 2018
    detail.hit.zdb_id: 2411122-3
    detail.hit.zdb_id: 2142091-9
    SSG: 21,3
    SSG: 14
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  • 8
    Online Resource
    Online Resource
    Wiley ; 2018
    In:  Water and Environment Journal Vol. 32, No. 3 ( 2018-08), p. 392-403
    In: Water and Environment Journal, Wiley, Vol. 32, No. 3 ( 2018-08), p. 392-403
    Abstract: Soil erosion is a major environmental problem. Vegetation, on the other hand, plays an important role in controlling soil erosion. The goal of the study is to examine the effects of the distribution pattern of vegetation on water flow. The vegetation parameters involved included the direction of plant rows, plant stem diameter and row spacing. To study how vegetation affects the flow of water on slopes, flume simulation experiments were conducted using three different plant row directions, three different plant diameters and three row spacing. Experimental slope is fixed, slope ratio of 1.0%. The hydraulic characteristics of the slope under the three vegetation distribution patterns are explored. The results showed that the pattern of vegetation distribution significantly affected the resistance of vegetation to water flow and pattern on this slope. When the angle ( θ ) between plant row and water flow directions decreased, the plant diameter ( d ) increased, or the row spacing ( a × a ) decreased, the Darcy–Weisbach resistance coefficient ( f ) for water flow became larger. Simultaneously, the Reynolds and Froude numbers ( Re and Fr ) both became smaller. In experimental procedure condition, the change rate of f , Re and Fr were analysed by linear regression, the θ decreased every 10°, the average increase rate of f was 6.6%, the average decrease rate of Re and Fr were 2.0 and 3.0%. The d increased every 0.001 m, the average increase rate of f was 41.6%, the average decrease rate of Re and Fr were 11.2 and 12.2%. The a × a decreased every 0.01 m, the average increase rate of f was 45.2%, the average decrease rate of Re and Fr were 11.7 and 10.7%. The flow depth h increased every 0.01 m, the average increase rate of f and Re were 13.6 and 25.2%, and the average decrease rate of Fr was 10.4%. The experimental procedure results will be valuable for not only revealing the hydraulic characteristics of flow over vegetation land, but also the optimisation of the distribution of vegetation on a slope.
    Type of Medium: Online Resource
    ISSN: 1747-6585 , 1747-6593
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2018
    detail.hit.zdb_id: 2218235-4
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  • 9
    In: Colloids and Surfaces A: Physicochemical and Engineering Aspects, Elsevier BV, Vol. 695 ( 2024-08), p. 134199-
    Type of Medium: Online Resource
    ISSN: 0927-7757
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2024
    detail.hit.zdb_id: 1500517-3
    detail.hit.zdb_id: 1169792-1
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  • 10
    Online Resource
    Online Resource
    IOP Publishing ; 2022
    In:  Environmental Research Letters Vol. 17, No. 5 ( 2022-05-01), p. 055006-
    In: Environmental Research Letters, IOP Publishing, Vol. 17, No. 5 ( 2022-05-01), p. 055006-
    Abstract: Drought legacy effects of forest ecosystems have been widely observed. However, the influence of forest type and stock volume on its recovery path is poorly understood. In this research, we first used the Standardized Precipitation Evapotranspiration Index to identify a drought event. Then, we applied the normalized difference vegetation index deficit and forest property maps derived from forest inventories to investigate the potential impacts of forest properties on forest recovery paths. The results showed that the legacy effects 1–3 years after a drought event were pervasive, but the forest recovery path was highly dependent on the forest type and forest stock volume. The recovery of forests with low stock volume densities ( 〈 60 m 3 ha −1 ) was mostly stronger than that of forests with high stock volume densities (≥60 m 3 ha −1 ) by the second year. Although all forests with different stock volume densities approximately returned to a normal status by the third year, they followed various paths to recovery. Natural coniferous forests in China that have a similar stock volume density ( 〈 60 m 3 ha −1 ) took longer to recover than planted coniferous forests and exhibited a lower magnitude of recovery. These findings highlight that drought legacy effects are greater for natural coniferous forests with high stock volume densities, which provides insightful forest management information on how to speed up forest recovery with forest density control and type control.
    Type of Medium: Online Resource
    ISSN: 1748-9326
    Language: Unknown
    Publisher: IOP Publishing
    Publication Date: 2022
    detail.hit.zdb_id: 2255379-4
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