如果没有这些大量冷却的海冰，被带到北极的暖空气可以比以前更深入渗透到内陆。
Without those masses of cooling sea ice, warm air brought to the Arctic can penetrate further inland than it ever did before.
废水通过油脂分离器后汇入渗水坑。
紧实层的存在影响地表入渗和坡面产流产沙量。
The density horizon may influence the content of sediment in the runoff.
20世纪以来，入渗与产流研究取得了长足进展。
Since the 20th century, a great progress has been made in research on infiltration and runoff yield.
土壤入渗性能是评价土壤水源涵养功能的重要指标。
Soil permeability is an important index of evaluating water source conservation function.
地下水主要补给来源为大气降水的入渗和地表水体的渗漏。
Groundwater recharge mainly comes from infiltration of precipitation and seepage of surface water.
且随着PAM覆盖度的增加，入渗率与稳定入渗率也增加。
With the PAM coverage increased, infiltration rate and stable infiltration rate are also increased.
经过模型检验、参数反演，确定了水力参数和入渗补给系数。
The hydraulic parameters and infiltration supplement coefficient are ascertained by model testing and parameter inversion.
在此基础上进行了西郊地区河道入渗和砂石坑入渗模拟研究。
After that, river way influent seepage and sand pit influent seepage simulation are researched at western outskirt in Beijing.
这些研究成果为进一步研究点源入渗和膜上灌技术奠定了基础。
These research results have laid a foundation for further research of point source infiltration and film hole irrigation.
波涌沟灌条件下土壤水分入渗研究是实现精量灌溉的理论基础。
The study on soil water infiltration under surge irrigation is the thesis base of applying accurate irrigation.
因此，对浑水入渗滞留的研究有助于全面认识浑水的入渗过程。
Therefore study on the detention is helpful to understanding whole infiltration of muddy water.
国内外相关研究集中于沉积对入渗的影响，忽略了入渗滞留的作用。
The study on this problem is concentrated on the effect of sediment and neglect that of detention.
在整个入渗过程中，土壤水分入渗性能随着开垦年限的延长呈下降趋势。
The permeability of soil showed downtrend along with the period of tillage prolonged during the whole infiltration process.
供水入渗过程中，浓度锋运移距离和浓度最大值均随时间的延长而增大；
The concentration front transport distance of and the maximum value of concentration increased with increased time in the process of water supply.
降水入渗规律的研究可为流域水文过程的预测和评价提供重要的科学依据。
Study of water through soil infiltration may offer a scientific support for prediction and evaluation of watershed hydrological processes.
本文研究均质土壤、表面供水强度已知但未超过土壤入渗能力的入渗模型。
This paper deals with an infiltration model in which rainfall or sprinkling intensity are known but it is less than the infiltrability of soil.
将土-水-气三相耦合，提出了一种确定降雨入渗后的暂态渗流场的模型。
A model for confirming this infiltration field is presented by soil, water and atmosphere three-phase coupling.
土壤入渗性能对水资源转换利用、农业水管理等方面有着十分重要的作用。
Soil infiltrability is an important issue in water resources transformation and utilization as well as agricultural water management.
以上成果为进一步研究膜孔肥液入渗的影响因素和灌水技术提供了理论基础。
These researches have laid a foundation for further study of the influence factors in film hole fertile solution infiltration.
水的入渗能对土体强度产生较大的影响，它是造成边坡破坏的一个主要因素。
Water is a key factor to slope's stability, which has a strong effect on the strength of soil.
土壤入渗通用公式与实测曲线在入渗衰减阶段的入渗过程最为相似，拟合较好。
The current formula of soil infiltration was similar to infiltration process in the initial phrase and can simulate total infiltration process better.
随着降雨雨型的变化，土壤入渗速率依时间变化曲线与常态有压入渗时迥然不同。
The curve of soil infiltration rate with time is different greatly from that of normal infiltration in press.
基于大田土壤入渗试验，讨论了玉米秸秆覆盖对土壤冻融特点及入渗能力的影响。
Based on soil field infiltration test, the effects of corn straw mulch on freezing-thawing soil infiltration capacity are discussed.
同时，地表水一旦入渗墙后土中，则可以通过砌体较快地排出，有效降低地下水位。
At the same time, once the surface water infiltration wall in soil, can be discharged through the masonry quickly, effectively reduce the ground water level.
因此，可以认为入渗系数主要取决于垃圾体剖面的结构特征，与降雨条件关系不大。
Therefore, it can be concluded that permeating coefficient of precipitation is mainly decided by the section character of garbage body and no relation to rainfall.
水分的脱盐效率随淋洗水量的增加呈幂函数减小，随入渗水矿化度的增加线性减少。
The water-desalting efficient decreased exponentially with increasing leaching water volume and linearly with water salinity.
水分的脱盐效率随淋洗水量和入渗水矿化度的增加而减小，与土壤初始含水量无关。
The desalting efficiency of saline water decreased with increasing amount of leaching water and the concentration of saline water, but was independent of initial soil water content.
水分的脱盐效率随淋洗水量和入渗水矿化度的增加而减小，与土壤初始含水量无关。
The desalting efficiency of saline water decreased with increasing amount of leaching water and the concentration of saline water, but was independent of initial soil water content.
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