slope length meaning in Chinese
坡长
Examples
- With the same slope gradient and slope length , the soil erosion on the dyke slope caused by the runoff mainly depended on the factors such as the runoff , flow velocity , rainfall intensity , rainfall duration , as well as the up - slope drainage area of dyke slope
坡度、坡长一定时，径流对戗坡的侵蚀主要与径流量、流速、雨强、降雨历时，戗坡以上汇聚水量或集水面积有关。 - A solid - waste containment system can be simplified as a slope which contains a layer of geomembrane ( which is simplified as interlayer slope in the rest part ) . shaking table model test and numerical analysis have been done to study the seismic stability of interlayer slope based on the two - part wedge theory in this paper . many factors which affect the slope stability ratio , including horizontal seismic coefficient , slope angle , soil - geomembrane interaction coefficient , slope length , layer thickness and soil character , have been took into consideration
填埋场防渗基坑的边坡可以简化成含土工膜夹层的土坡(以下简称夹层土坡) ，本文根据“双滑楔体”理论思想，对夹层土坡的地震稳定性问题进行了较为系统的模型试验和数值分析，着重考虑了水平地震系数、夹层土坡坡角、土工膜与覆盖层土体摩擦系数、夹层边坡长度和厚度、夹层土坡覆盖层土体性质等因素对土坡安全系数的影响，并对地震作用下夹层土坡的永久变形进行了初步的研究，给出了对实际工程设计有参考价值的结论。 - According to climate condition , soil condition and afforesting tree species and water requirement rule of forest and grass , the paper analysed and calculated the slope length for collecting stream of three site preparation methods which were reverse - slope terrace , level trench and scale - hole , and the slope length for collecting stream of deferent gradients and planting bandwidths were acquired
摘要根据宁南山区的气候、土壤、造林树种等，按照林草植被建设的水分需求规律，对不同水上流失区的反坡梯田、水平沟、鱼鳞坑3种整地方式的集流坡面长度进行分析与推算，计算出了不同坡度、植树带宽度下的集流坡长。 - The topographic feature is one of the main factors that influence the process of soil erosion and sediment yield of small watershed . the quantitative parameters of small watershed topographic feature are average watershed slope , average slope length , gully density and so on , which are based on the quantitative method of slope character and do not reflect the essential character of the small watershed topographic feature , which are complex
地貌形态是影响小流域侵蚀产沙的主要下垫面因素之一，其量化参数一般继承坡面地貌特征量化方法(如坡度、坡长因子)而采用平均坡度、平均坡长及沟壑密度等参数，这些参数仅是对流域地貌形态的概化和单因子表达，没有真正反映流域地貌形态复杂的本质特征和相互联系。