DRO：直接径流

“Direct RunOff”在学术与科研领域，尤其是在地质学相关研究中，常被缩写为“DRO”，以便于快速书写和日常使用。这一术语的中文释义为“直接径流”，通常指降水或融雪后未经过下渗而直接汇入河流、湖泊等地表水体的水流过程，是水文学与地质学中的重要概念。

In order to process data of direct runoff and water infiltration through soil from field tests, curve-fitting techniques were used.
为了处理在野外测试中得到的地表径流和土壤渗透资料，采用了曲线拟合方法。
The differences of the direct runoff of rainwater among different landscapes of hillside fields provide basis and controllability for the utilization of rainwater on hillside fields and for using hillside fields to collect rainwater to support farmland irrigation.
坡地不同垫面间雨水地表径流的差异存在，为坡地雨水利用和利用坡地集雨支持农田灌溉提供了依据和可调控性。
The direct runoff flow at the outlet was the sum of the volumetric flow from all cells arriving at the outlet at each respective routing time.
出口的直接径流(DRO)就是在各个汇流时间段内到达出口的所有格网单元的体积流之和。
In the east, the water is mainly oceanic with relatively minor dilution from direct monsoonal rainfall and runoff from small streams.
东部水域主要为海水，而直接的季候雨及小溪溢流，把海水稍为冲淡。
The water absorption character of geotextile have a direct impact on the runoff process. The paper studies the water absorption of straw, jute, palm, palm-leaf by the indoor method.
地表覆盖物的吸水特性直接影响径流的产生过程，通过室内研究方法，研究了稻草、黄麻、棕榈、棕榈叶的吸水特性。

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