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stored water
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  储水
     Results Iodine content varied in the different state of stored water.
     结果不同储水状态碘含量不同;
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     Iodine content varied with the state of stored water and the number of iodinator.
     碘含量随储水状态、释放器数量变化而变化。
短句来源
     Study on Mechanism of Water-saving and Benefit-increasing of Irrigation with Stored Water in Shallow Groundwater Areas
     地下水浅埋区储水灌溉节水增效机理研究
短句来源
     The application of the irrigation with stored water can not only regulate the inhomogeneity of the water distribution in the year, but also increase the use factor, improve the water consuming environment, promote the virtuous circle of water resources, achieving the goal of saving the water and increasing the benefit.
     利用储水灌溉可以调节年内水量分配的不均匀性 ,也可以利用储水灌溉提高水的利用率 ,改善用水环境 ,促进水资源良性循环 ,达到节水增效的目的
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     Objective To know about and master the present tunnel stored water quality of our army. To present the tunnel water disinfecting effect by making use of controlling-released potable water disinfectant (CRPD) so as to offer scientific evidence to the potable water disinfection.
     目的 了解我军部分坑道现有储水的水质状况 ,评价坑道储水施用控制释放饮水消毒剂 (CRPD型 )的消毒效果 ,为饮水消毒提供科学依据。
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  储水量
     The stored water of the plantations was all decreased at the end of the growing season compared with that at the beginning, P. tabulaeformis, P. sylvestris var. mongolic and C. microphylla decreased by 17 mm, 8 mm and 73 mm respectively. More water was consumed by C.
     在季节变化上,柠条林地土壤含水量最高值出现在生长季以前,油松、樟子松林地土壤含水量最高值则出现在6、7月份,在生长季末各林地储水量均低于初期,油松、樟子松、柠条林地分别减少了17mm、8mm和73mm,柠条的耗水量大于油松和樟子松。
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  “stored water”译为未确定词的双语例句
     Water level in the iced reach is generally dammed up 1. 1 to 1. 8 meters with flood area of about 160 km2 over two dykes, and stored water of 134 million m3.
     封冻河段水位普遍壅高11-1.8m,两岸滩区冰水漫溢,受淹面积约160km2,滞蓄水量1.34亿m3。
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     The results showed that under no irrigation, winter wheat used mostly water of 20~60 cm soil layers, and increased the consumption of soil stored water by 96.84 mm;
     结果表明,在非灌溉条件下,冬小麦主要利用20~60 cm土层中的水分,冬小麦对土壤贮水的消耗量增加,平均多耗水96.84 mm;
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     Rainwater utilization & preventing cold loss and saving energy in using roof stored water
     城市雨水利用与蓄水屋顶防热节能
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     The difference between the simulated cumulative evaporation and that measured using micro lysimeter in 18 days was less than 0.7mm. The difference of stored water in the profile of 0 ̄23cm between simulation and measurement was less than 4mm.
     模拟数据与同期用micro-lysimeter测定的数据相比较,测定期间18d的累积蒸发量相差在0.7mm以内,0~23cm剖面上的土壤贮水相差在4mm之内,但模拟的土壤温度比实测偏高,特别在清晨。
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     How will be the developing trend of debris flow activity after the level of stored water in the reservoir reaches a height of 175m in 2009?
     2009年水库175m水位蓄水后,泥石流活动的发展趋势如何?
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  stored water
A method of calculating the freezing of stored water in seasonally frozen ground
      
The implementation of a Wholesale Water Market is proposed for trading stored water and so to correct such distortion.
      
A novel scheme is presented for modeling the constraints to preserve the reserved stored water in (directly and non-directly) upstream reservoirs to satisfy potential future needs in demand centers at given time periods.
      
The loss of stored water from surface water reservoirs through evaporation is inevitable and can be significant in arid and semi-arid climates.
      
Close to the branch, evaporation of stored water in humus cools the environment while latent heat transformation on epiphyte surfaces raises temperature.
      
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Since the year 1886, the Dupuit-Forchheimer theory and formulas for gravityflows toward wells and galleries have been broadly used in all nations of theworld. In these formulas, assumptions are made for underground flows fromfarther distances in horizontal directions at a constant rate toward wells andgalleries. According to the author's analysis, these assumptions are not consistentwith the actual conditions of flow, hence the formulas obtained therefrom are notrational, and the employment of these formulas...

Since the year 1886, the Dupuit-Forchheimer theory and formulas for gravityflows toward wells and galleries have been broadly used in all nations of theworld. In these formulas, assumptions are made for underground flows fromfarther distances in horizontal directions at a constant rate toward wells andgalleries. According to the author's analysis, these assumptions are not consistentwith the actual conditions of flow, hence the formulas obtained therefrom are notrational, and the employment of these formulas to investigate the general effectof surface drop or well diametre upon yield is devoid of rational foundations. According to the author's analysis, the flows toward wells or galleries areactually supplied vertically by draining the stored water above the free surface inthe course of its descending and enlarging. As the drainage of gravity water fromthe pores of soil particles in order to reduce the water content to that of filmshells takes one to two days, as the capillary water columns are interconnectedand mutually supplied sidewise, this vertical supply of water may maintain quite along time, yet the flow may not be absolutely steady. As regards vertical supply of water with unsteady regimen, equations of freesurface for flow pattern near galleries are deduced, corresponding to the Boussinesqpartial differential equation. Besides, the author has derived simplified equationsfor computing flows into wells and galleries. The latter, in comparison with theDupuit-Forchheimer formulas, gives a higher yield, while the free surface curve isreasonably tangent to the horizontal water table at a point which moves fartheraway as time goes on. J. Kozeny first pointed out the phenomenon that the water depth in the groundon the wall will not be further lowered when it reaches one half of the depthbefore pumping. The author hereby proposes a theoretical proof of it on the basisof theorem of least work. Based upon these theories, formulas are proposed for maximum possible yieldof wells and galleries dug to horizontal impervious strata, to be used in prelimi-nary estimations for hydro-geological workers.

1886年以来,杜布义-福熙罕默(Dupuit-Forchheimer)的井流及沟流的理论与计算用公式被世界各国广泛地应用着。公式假设地下水从远处沿着水平方向以定率流向井内或沟内,按作者分析这种假设并不符合实际情况,因之所得公式也不合理,用这些公式来推论水位降落或井径对於出水率的影响也没有合理的凭据。作者推论,井流或沟流的水实际上是从水面线以上,在其降落并扩大的过程中,排除了存积的水,沿着直垂方向所供应着的。因为从土壤颗粒的空隙间排除重力水,使减为薄膜水,每需时一两天,而水面上的毛细管水又是横向贯通并互相接济着,所以垂直供水可以维持很久,而潜流也决不会绝对稳定。根据这垂直供水的不定汉条件引出了沟流的水面线公式,结果符合蒲薪奈斯克的偏微分方程式。另外,作者又拟具了简化的井流及沟流计算用公式。这些公式和杜氏-福氏公式比较,所得出水率较大,而水面线则合理地切於静水线,切点随着时程向远处移动。柯臣尼(J.Kozeny)最早指出井边地内水深不会低於静水深一半的现象,本文中作者根据最小工作定律试拟了理论的证明以支持之。根据这些理论,引出了从静水中抽水时井流、沟流最大可能出水率的公式,以供水文地质工作者初步估算之用。

The paper deals with the No. 22 crossing faults' data of the mobile levelling measurement by use of Fourier analysis method, showing that the original compressional reverse fault crossed the reservoir has got active feature of the similar normal fault after stored water at Sikouzi reservoir. Through further analysis, it is considered that this may be the results of buoyancy of pressure water, regional compressional tectonic stress and quiet pressure of water load, where the buoyancy of pressure...

The paper deals with the No. 22 crossing faults' data of the mobile levelling measurement by use of Fourier analysis method, showing that the original compressional reverse fault crossed the reservoir has got active feature of the similar normal fault after stored water at Sikouzi reservoir. Through further analysis, it is considered that this may be the results of buoyancy of pressure water, regional compressional tectonic stress and quiet pressure of water load, where the buoyancy of pressure water is playing the important part in the fault motion at the reservoir area.

本文利用带线性项的富氏多项式最小二秉拟合分析法,处理了寺口子水库区22期跨新层流资料。结果表明,在寺口子水库蓄水后,穿过库区的原压性逆断层,具有了似正断层的活动特征。进一步分析认为,这是由于压力水的浮力、区域挤压构造应力和水体载荷静压力共同作用的结果,而压力水的浮力在库区断层活动中起着主导作用。

The main problem for crop production on the drylaud of semi-arid regions in China is the Shortage of available water, and therefore the soil management is concentrated in water management. Full storage of water in soil, ratilonal utilization of it, and reservation of the stored water as much as possible are the startnig point and end-results of the soil management.Levelling lands, ploughing, mixing some sandy soil with clay soil or clay soil with sandy soil, and taking effectiye drought-relief tillage...

The main problem for crop production on the drylaud of semi-arid regions in China is the Shortage of available water, and therefore the soil management is concentrated in water management. Full storage of water in soil, ratilonal utilization of it, and reservation of the stored water as much as possible are the startnig point and end-results of the soil management.Levelling lands, ploughing, mixing some sandy soil with clay soil or clay soil with sandy soil, and taking effectiye drought-relief tillage have played a great role in increasing water percolation of soil and reserving water in soil. The tillage pracljces worthy of mention here are cultivation in pits and cultivation in furrows. The two metheds were used as early as in the Han dynasty and have been tested and improved.The procedure of the furrow cultivation is as follows,digging land to make furrows at a certain distance,deep ploughing the furrows,cracking the soll blocks,compacting the loose soil and smoothing the surface,and then Planting crops in the furrows. The soil dugout from the furrows is used to make ridges. The ridges and the rest of the field retain fallow or are usad to plant green mannre crops. After harvest of the crops,the furrows are moved to the place next the primary ones. In this way, through about 3 to 4 years, all the soil in the land has been used as furrows and improved.The pit cnltivation has the same procedure as the former except digging pits instead of furrows. Experiments showed that. by digging furrows or pits, soil water and grain ylelds were increased significantly.Nore attention has been paid in the dryland farming to using as much as possible the water stored in soil and making the water produce the greatst efficiency of production. Raising soil fertility is more inportant for inereasing the production afficiency of precipitation Application of fertilizers,use of rotalion, fallow and planting green manure crops can raise and recover soil fertility,making soil water more efficient. Also, the use of drought-resis tent crops and adoption of suitable method for seeding under the condition of laking moisture in soil can make use of the limited water to the fullest extent.Reserving stored water in soil as long as possible has attracted attention in dryland soil management. Such measures as rolling lands when soil moisture is deficient,loosing and raking soil when soil is wet, hoeing after rain and mulching with sand and gravels can diminish losses from evaporation and have so far played an important role in dryland agricul tural production.

旱地土壤管理的核心是水分管理。充分蓄水、合理用水、千方百计保水是管理的出发点和归宿。我国旱农在这方面有着丰富经验。平整土地、蓄水耕作(如沟种和坑种)、深耕、客土调剂等,均能增强水分就地入渗、在蓄纳降水方面有重要作用。合理施肥、采用轮作、休闲,种植绿肥等措施,提高或恢复土壤肥力,能充分发挥水分的增产效益,选用抗旱作物,巧用地墒播种能使有限降水得到合理利用。墒欠镇压,趁墒耙耱,雨后中耕,以砂覆盖等措施,能减少水分蒸发损失,至今仍在旱农生产中发挥着作用。

 
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