地表径流量的英文

• direct runoff rate

• "地表径流"英文翻译    surface runoff
• "量"英文翻译    measure capacity
• "表流；地表径流" 英文翻译 :    surface flow
• "地表径流" 英文翻译 :    direct runoff; direct surface rnn off; direct surface runoff; flowing sheet water; flowing surface water; immediate runoff; land－runoff; overland flow; overland runoff; overlandrunoff; rainwash; runoff flow; sheet runoff; surfacerunoff
• "地表径流率" 英文翻译 :    rate of surface runoff
• "地表径流水" 英文翻译 :    running off water; surface runoff water
• "地表径流长度" 英文翻译 :    length of overland flow
• "地表径流系数" 英文翻译 :    coefficient of surface runoff; surface runoff coefficient
• "地表径流地面径流" 英文翻译 :    surfacerunoff
• "地表径流直接径流" 英文翻译 :    direct runoff; directrunoff
• "地面径流；地表径流" 英文翻译 :    surface run-off
• "地表径流过程线" 英文翻译 :    overland flow hydrograph
• "地表径流形成期" 英文翻译 :    net supply interval
• "表径流" 英文翻译 :    flow of ground
• "地表径量" 英文翻译 :    surface discharge; surface run off
• "径流量" 英文翻译 :    river runoff; runoff amount; runoff volume; volume of runoff
• "年径流；年径流量" 英文翻译 :    a ualrunoff; annual runoff
• "地表暴雨径流" 英文翻译 :    spate flow; spate runoff
• "单位径流量" 英文翻译 :    unit runoff
• "固体径流量" 英文翻译 :    sediment yield; silt load; solid discharge
• "河流径流量" 英文翻译 :    river runoff
• "洪峰径流量" 英文翻译 :    peak runoff
• "季径流量" 英文翻译 :    seasonal flow; seasonal runoff
• "径流量测槽" 英文翻译 :    runoff-measuring flume
• "径流量峰值" 英文翻译 :    peak rate of runoff

• Furthermore , soil and water conservation also resulted in the underground flow decrease but its decrease extent is smaller than of surface flow
  水土保持也使河川地下径流量有所减少，但降低程度较地表径流量小。
• Increased surface runoff was found in the mountainous areas of the southwest and northeast , and in some areas along the south coast
  地表径流量升高的地区以西南部及东北部高山地区较为明显，在南部沿海部分地区亦有类似现象。
• And we have got the following result : 1 . the technique of storing water in soil in gneiss area of tai - hang mountain : the more water in soil before rain is , the less water capability of soil is , the time shorter of water flowing from soil is , the easier the water flows on the ground ; the soil capability of reserving water of different soil thickness is terrace > acacia land > pine land > grass land , so the soil is more thick , the soil capacity which contains water is more large ; the accumulated water that flows on the ground is remarkable related with the logarithms of rain time
  太行山片麻岩区土壤蓄水规律：雨前土壤含水量越高，土壤可蓄水量越小，出流所需时间越短，容易形成地表径流；不同土层厚度的土壤蓄水量为：梯田刺槐林地油松林地草地；累积地表径流量与降雨时间的对数呈显著正相关，拟合方程为w = a + blnt ，相关系数均大于0 . 92 ，即在降雨强度一定的前提下，降雨时间越长，累计地表径流量越多。
• The paper studies on two different vegetation type areas in jingyun mountain in chongqing city , which are broadleaved forests ( gordinya svchuanensvs ) and bamboo ( phyllostachys edulis ) forests . by contrasting the surface runoff and underground runoff in these two areas , the results showed that , with the same precipitation , the gross amount of runoff in bamboo forests was larger than that in broadleaved forests and the runoff in bamboo forests appeared before that in broadleaved forests . the amount of underground runoff was larger than that of surface runoff in the two areas , the process of surface runoff was in accordance with that of underground runoff
  该文以重庆市缙云山的两个不同植被类型常绿阔叶林(四川大头茶)和楠竹林小区为研究对象,对小区中典型降雨后的地表径流、地下径流的实测资料进行对比分析.结果发现在相同降雨条件下,楠竹林的地表径流量与地下径流量明显要比常绿阔叶林的大,楠竹林地表径流和地下径流出现的时间也比常绿阔叶林早;两种植被的地表径流与地下径流过程具有一定的相似性,地下径流量都比地表径流量大