But, in this case, no pumps meant no water movement.
但是,在这种情况下,没有水泵意味着没有水移动。
This is a water movement. I am moving like water.
般的动作。我向水一样的流动。
This adversely affects water movement, permeability, and aeration.
这对水分移动,渗透度及通气性有不利影响。
The plan consists of three elements: creating, growing and water movement.
该计划包括三个要素:创建,成长和水流运动。
Bend flow is a common phenomenon of water movement in channels and river course.
弯道水流是渠道和河道中常见的一种水流运动现象。
The water retention curve is one of the essential links to study the soil water movement.
土壤水分特征曲线是土壤水分运动研究必不可少的环节之一。
It is one of the common methods to study water movement in geological media using 3h as tracer.
用3H作为示踪剂研究水的运动是一种最常用的方法。
Soil water movement is mainly influenced by site type, vegetation and atmosphere precipitation.
土壤含水量的动态变化主要受大气降水、植被、立地等的影响。
These marker buoys assist RCC Australia by providing information about water movement to assist in drift modelling.
这些标记浮标可以通过提供关于水文运动的信息来协助澳大利亚海事安全局构建漂移模型。
A start of preferential research symbolizes that mechanism of soil water movement is from homogeneous to heterogeneous field.
开展优先流研究,是土壤水运动机制研究由均质走向非均质领域的标志。
Spatial variation pattern of water movement parameters in unsaturated soil is the base of parameter estimation in a large area.
非饱和土壤水分运动参数的空间变异规律是大区域参数估计的基础。
The mathematical model of solute and water transport is composed of two coupled equations of water movement and solute transfer.
土壤水和溶质迁移的数学模型,可分别由水分运动、溶质运移两个方程耦合组成。
The paper analyzed the characteristics of the soil water movement of drip irrigation under mulch in different cropping patterns.
从土壤水流动系统的角度分析了膜下滴灌不同种植方式下土壤水流动系统特征。
If the water is serious, should be taken immediately to a watch shop to clean oil, clear water movement, to avoid the parts rust.
如果进水严重,应立即送往表店擦油,清楚机芯里的水分,以避免部分零件生锈。
Soil water retention characteristics served as a vital parameter in modeling water movement and chemical transport in unsaturated soil.
土壤水分特征曲线是模拟水分和化学物质在非饱和土壤中运移的关键参数。
Preservative law of geothermal resources of Yongchun is result of ground water movement under controlled by special geological structure.
永春地热田热资源赋存规律是其特殊地质构造制约地下水运动的结果。
The hydrology is a science to study natural water movement, the change state and rule of the water quantity and quality in time and space.
水文是研究自然界水的运动、水的数量和质量在时间和空间上变化状况及变化规律的一门学科。
This paper introduces the research method and contents of the law of soil water movement, and probes into some problems needing future research.
介绍了土壤水分运动规律研究方法及内容,探讨了需要进一步研究的问题。
The paper deals with the law of ground water movement in the slope and analyzes the effect of high phreatic line in the bulk on the slope stability.
本文从研究边坡中地下水运动规律入手,分析坡体中的浸润线位置过高对边坡稳定的影响。
Research on reservoir flow units may better understand the rule of oil-water movement and distribution of remaining oil during the development process.
储层流动单元的研究可以更好地了解油水运动规律及开发过程中剩余油的分布。
The research at home and abroad on the simulation of soil water infiltration equation soil water movement parameters and the theory of SPAC were reviewed.
论述了国内外在土壤水分入渗方程模拟、土壤水分运动参数和SPAC理论等方面的研究进展。
Theoretical analysis of local-control irrigation, i. e. , non-pressure underground irrigation, is conducted, and soil water movement equation is presented.
对局部控水灌溉(无压地下灌溉)技术从理论上进行了分析,并给出了其土壤水分运动方程。
Derivation soil hydrodynamic parameter and numerical simulation of soil water movement and distribution are important parts of soil water movement research.
土壤水动力学参数的推导和土壤水分运移分布的数值模拟是研究土壤水分运动规律的重要部分。
Soil water movement and solute transport in the local scale were studied and the spacial variability of soil water content and concentration were discussed.
据此研究了小区域范围内土壤水分和溶质的运移特征,讨论了土壤水分和盐分分布的空间变异性和统计特征。
The DRASTIC method can provide groundwater vulnerability to pollution but does not contain risk concept and ignore hazard's dynamic nature of water movement.
DRASTIC方法可以进行地下水污染的脆弱性评价,但是却没有涵盖风险的概念,也忽视了污染物随地表水流运动的动态特性。
The dynamic laws governing the water movement in unsaturated zone provide a reliable theory for water transform, water saving and groundwater formation and ullage.
非饱和带水分运移规律的研究对“四水”转化研究、节水研究、地下水资源的形成与损失研究等提供了可靠的理论依据。
Spatial variability of soil water retention function is a primary prerequisite for quantitative research on water movement and solution transfer in unsaturated zone.
土壤水分特征函数空间异质性是定量研究土壤非饱和带水分运动以及溶质运移的先决条件。
Through the laboratory research and field experiment, the influencing mechanisms of lateral depth in non-pressure irrigation on soil water movement and crop growth are studied.
通过室内试验和大田试验,研究了无压灌溉方式下埋管深度对水分运移和作物生长的影响机理。
This paper presents a mathematical model which involves only four parameters to simulate the water movement and balance of surface and groundwater in a basin or an irrigation area.
本文提出一个仅含四个参数的数学模型来模拟一个流域或泄区的地面水和地下水的运动及水量平衡情势。
This paper presents a mathematical model which involves only four parameters to simulate the water movement and balance of surface and groundwater in a basin or an irrigation area.
本文提出一个仅含四个参数的数学模型来模拟一个流域或泄区的地面水和地下水的运动及水量平衡情势。
应用推荐