1) rate of rise
水位上升速率
1.
Based on three important parameters such as weight of hydrological zones (HZ), depth to water (DTW) and rate of rise(RR), a hydrological response units (HRU) map 2001 was created in the Tao’er River basin, Songnen plain, which can response sensitively to the spatial change of groundwater environment, and it is produced by the algebraic multiplication of the three classified grids: HRU = DTW*RR*HZ.
运用水文响应单元(HRUs)法评价洮儿河流域地下水环境空间变化对盐渍化风险等级的影响过程,利用反映地下水环境空间变化的3 个重要参数:水文区权重(HZ)、水位埋深(DTW)和水位上升速率(RR),由其3个等级网格值算术相乘HRU = DTW*RR*HZ在GIS 平台上生成2001 年水文响应单元图。
2) the critical rise rate of waterhead
临界水位上升速率
3) rise of water level
水位上升速度
4) rising velocity of the water level
水位升高速率
5) rising rate
上升速率
1.
First, the constant-speed stage during the phase separation of aqueous two-phase system in static circumstance was properly hypothesized, and the framework of the rising rate model for dispersed phase droplets was established via mechanical analytical method.
对静态环境中双水相系统相分离过程的恒速阶段进行了适当的模型假设,并采用机理分析方法建立了分散相液滴上升速率模型。
6) relative increase of speed
速率上升
补充资料：地下水水位观测(见水位观测)
地下水水位观测(见水位观测)
d ixiashui shuiwei guanee地下水水位观测见水位观测。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条