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Gully Growth Patterns and Soil Loss under Rainfall at Urban Underground Drainage Construction Site, Uyo

机译:于阳县城市地下排水施工现场雨水沟壑生长方式及土壤流失

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This study investigated, evaluated and modeled patterns of growth of gully morphometric dimension and soil loss volume under prevailing rainfall on the slopes of land graded for the construction of underground drainage at Uyo but delayed in completion. Land grading at underground (tunnel) drainage construction site rendered the exposed surface very impervious but young ephemeral gullies developed due to delays in completion. Data on gully morphometric dimension, soil loss and depth of rainfall were analyzed using SPSS ver. 17 statistical package. Mean gully growth in length, width and depth were different at 2.54±0.86, 0.923±0.29 and 0.41±0.11 m, respectively, yielding 3.87±0.08 m2 as mean volume of soil loss at full stage. Cubic polynomial was best-fit model for growth in length (R2 = 79%) and width (R2 = 69%) using weekly rainfall for an annual season. All gully sites had constant depth change, better predicted by quadratic (R2 = 13%) than linear (R2 = 9%) functions. Mean volume of soil loss per unit rainfall amount varied with low, medium and high rainfall amount and was highest at slope bottom (33 cm3/cm) and least at the crest (6.99 cm3/cm) with R2 = 38-34%. Land grading to impervious sublayer produced constant depth change in all gullies at the sites. The models for morphometric incremental growth and soil loss volume under the rainfall effect was significantly improved (p2 = 91-99%). Rainfall was the principal gully factor and construction delays should be avoided.
机译:这项研究调查,评估和模拟了Uyo地下排水沟分级坡地上主要降雨条件下沟形形态尺寸和土壤流失量的增长模式,但该工作完成被推迟。地下(隧道)排水施工现场的土地平整使裸露的地面非常不透水,但由于施工延误而形成了年轻的临时沟壑。使用SPSS ver.1来分析有关沟渠形态尺寸,土壤流失和降雨深度的数据。 17个统计包。平均沟长,宽度和深度的差异分别为2.54±0.86、0.923±0.29和0.41±0.11m,全季平均土壤流失量为3.87±0.08m 2 。三次多项式是使用年度季节的每周降雨量的长度(R 2 = 79%)和宽度(R 2 = 69%)增长的最佳拟合模型。所有的沟壑位置都有恒定的深度变化,与线性函数(R 2 = 9%)相比,二次函数(R 2 = 13%)能更好地预测。每单位降雨量的平均土壤流失量随低,中,高降雨量的变化而变化,在坡底(33 cm 3 / cm)和最低峰(6.99 cm 3)最高 / cm),R 2 = 38-34%。土地平整为不透水的子层会在站点的所有沟渠中产生恒定的深度变化。降雨作用下形态计量增长和土壤流失量模型得到了显着改善(p2 = 91-99%)。降雨是主要的沟壑因素,应避免施工延误。

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