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Influence of the ground flora on the variation characteristics of the runoff distribution on red soil slope

Ecological Economy 2018年第2期11卷 109-116页

作者： CHEN Zhi HUANG Chao-long Faculty of Environmental Science and Engineering Kunming University of Science and Technology First Hydrogeological and Engineering Geological Brigade Yunnan Geology and Mineral Resources Bureau

In this paper, we use the inter flow area as the research object in the logical science park for soil and water conservation in Jiangxi province; and the Paspalum natatum and its litter cover are used as the ground flora. We discusses and analyses the vertical distribution of runoff so as to provide theoretical support for the wide application of the Paspalum natatum for soil and water conservation in the region of red soil in south China.

关键词： red soil slope ground flora runoff distribution

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Comparing the impacts of mature spruce forests and grasslands on snow melt,water resource recharge,and run-off in the northern boreal environment

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International Soil and Water Conservation Research 2015年第1期3卷 50-56页

作者： JiříKremsa Josef Křeček Eero Kubin Watershed Authority of the Elbe River Víta Nejedlého 951/8CZ-50003 Hradec KrálovéCzech Republic Department of Hydrology Czech Technical University in PragueThákurova 7CZ-16629 Prague 6Czech Republic Natural Resources Institute Finland Natural Resources and BioproductionPO Box 413FI-90014 University of OuluFinland

Snow-melt runoff is an important factor in control of flooding and soil erosion in higher and cold regions of the *** 1992-2008-2008,processes of snow accumulation and melting were monitored at two adjacent sites of the Paljakka environmental research centre(Finland).The forest stand of mature spruce(Picea abies)has been compared with adjacent,local,and open *** the forest,snowpack duration fluctuated for 180-245 days,with a maximum depth of 78-152 cm and snow-water content of 167-406 mm,while in the open grassland this occurred for some 20 days less,with maximum depth 65-122 cm,and snow-water content 143-288 *** snow-water captured in the canopy reached a maximum 27%of that registered on the ground;the loss of intercepted snow by sublimation was approximately 26% of the annual *** the high melt period(April-May),the degree-day factor in the forest stand achieved 60%of values observed in the grassland(2.3-3.5 against 3.8-6.0 mm℃^(-1)day^(-1)).The hydrological model BROOK 90 was employed to analyse potential water resources recharge,and flood risk at *** the normal climate season,snow-melt runoff from the forest exceeded the grassland by 22%(225 against 185 mm).In extreme situations,the maximum daily runoff from snow-melt in the grasslands(57 mm day^(-1))exceeded 2.6 times the values in spruce forest(22 mm day^(-1)).

关键词： Spruce boreal forest Snow-depth Snow-water content Canopy interception Snowmelt Degree-day factor BROOK 90 runoff distribution

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