过程线的英文

• hydrograph

• "过程"英文翻译    process; procedure; transver ...
• "线"英文翻译    thread; string; wire
• "充水过程线" 英文翻译 :    filling curve; filling hydrograph
• "单位过程线" 英文翻译 :    unit graph; unit hydrograph
• "单元过程线" 英文翻译 :    element hydrograph
• "典型过程线" 英文翻译 :    tyic hydrograph; typical hydrograph
• "分配过程线" 英文翻译 :    distributor graph
• "复合过程线" 英文翻译 :    compound hydrograph
• "过程线放大" 英文翻译 :    hydrograph enlargement
• "过程线分割" 英文翻译 :    hydrograph separation
• "过程线峰段" 英文翻译 :    peak segment
• "过程线合成" 英文翻译 :    hydrograph synthesis; synthesis of hydrograph
• "洪水过程线" 英文翻译 :    flood hydrograph; flood hygrograph; flood profile; floodhydrograph
• "降雨过程线" 英文翻译 :    hyetograph
• "进水过程线" 英文翻译 :    inflow hydrograph
• "亏耗过程线" 英文翻译 :    depletion hydrograph
• "亏水过程线" 英文翻译 :    depletion hydrograph
• "量过程线" 英文翻译 :    discharge hydrograph
• "流量过程线" 英文翻译 :    discharge curve; discharge hydrograph; flow duration curve; hydrograph curve of discharge
• "入流过程线" 英文翻译 :    inflow hydrograph
• "设计过程线" 英文翻译 :    design hydrograph
• "水位过程线" 英文翻译 :    level hydrograph; stage hydrograph; time-stage curve
• "水文过程线" 英文翻译 :    hydrograph
• "梯形过程线" 英文翻译 :    trapezoidal hydrograph
• "温度过程线" 英文翻译 :    thermogram

• Determination of flood control level hydrograph in chaershen reservoir
  察尔森水库汛限水位过程线的确定
• Base flow separation from daily flow hydrograph using automated techniques
  流量过程线的自动分割方法探讨
• The change of the characteristic sections of temperature process lines is analyzed and the coefficients obtained from analysis are used for comparison of the numerical simulation
  分析了特征断面的温度过程线的变化特点，得到的参数可供数值模拟对比使用。
• By use of many years ' hydrologic data , the max , water quantity dated from every day may be counted in every year ' s flood season , and the designed water quantity corresponds to the definite frequency
  滑动汛期水位在多年资料基础上，通过统计汛期中每日为起点的最大来水量，求出固定频率的设计来水量，选择合适的典型洪水过程线进行调洪计算后得到每天的汛限水位。
• And four constitutive models are established , which are hyperbolic model , half - logarithm model , exponential model and poisson model . combined with the analysis of the change of effective stress , the iteration formulations of settlement calculation are provided
  同时建立了双曲线模型、半对数模型、指数模型及泊松曲线模型四种本构模型，并结合有效应力过程分析给出了实用的沉降过程线的反演迭代公式。
• Observed tidal harmonic constants in many stations are used to verify the astronomical tides in the compound fluid model . the wave model is tested by a set of wave flume data at first . then the results are compared by the actual processes of significant wave height in gauging stations
  其中复合流场模型中的天文潮利用众多测站的实测调和常数进行验证；波浪模型首先进行了水槽实验的检验，然后在台风过程中，进行了测站有效波高过程线的比较。
• Mz , a , sk , kg and sc / d ( ratio of the sum of silt and clay to sand ) of fluvio - lacustrine , palaeosols and aeolian sands constitute an interlocking , multi - fluctuation process curve with peak and valle y values : the < & value of mz , o and sk values often increase accordingly from aeolian sands to its overlying fluvio - lacustrine facies or / and palaesols , the kg value heightens , too , and the sc / d value also basically consists with its change steps
  河湖相和古土壤与风成砂的mz 、 、 sk 、 kg以及sc d (粉砂粘土之和与砂的比值)构成一峰谷交替、犬牙交错的锯齿状多波动过程线：常常是由风成砂至上覆河湖相或和古土壤， mz的值、 、 sk值相应增大， kg相应增高， sc d值亦与之变化步骤基本一致。
• 1 - d and 2 - d model for non - uniform bedload transport are applied to compute the amount of bedload in the south branch of the changjiang estuary . it can be found that the peak value of bedload transport in a tidal cycle , computed by 2 - d model , is obviously larger than that computed by 1 - d model , which is induced by the disequilibrium of bedload transport in cross - river direction
  在此基础上，将非均匀推移质公式推广到二维计算，并与一维计算结果作了对比，发现两种计算所获得的净输沙量相差不大，但二维输沙过程线峰值较一维计算要大，这正是河道内推移质运动横向不均匀性的体现。
• Based on consider hereinbefore , this dissertation discusses several aspects on the problem of the sustainable and optimum exploitation of groundwater resources as follows : ( 1 ) reviewed entirely the origin and evolvement of the concept " sustainable development " , stated and commented the study status in queue on " sustainable development " around national and international range , thorough discussed the science connotation about the concept " sustainable development " ; ( 2 ) looked back and commented across - the aboard some furthest basic concept and proposition related to groundwater resources , put forward self opinions on a few existent mistake points of view and chaos understandings ; ( 3 ) expatiated entirely on the content and meaning of the theory of changeable groundwater resources system , contrast with the traditional methods of groundwater resources calculation and evaluation , combined example to show the application of this theory ; ( 4 ) thorough analyzed the difficult and complexity to forecast the groundwater resources , fully stated the traditional methods of groundwater resources forecasting , pointed out the characteristic and applying condition of these forecasting method , introduced the main ideas and methods of wavelet analysis developed recently , and the matlab software be known as the fifths era computer language , and its accessory wavelet analysis toolbox , applied these methods and tools to analyze the groundwater dynamic curve , adopted the b - j method and morte - carlo method , combined with the theory of changeable groundwater resources system , discussed the new view on the forecast of groundwater resources ; ( 5 ) synthetically analyzed the characteristics and limitations of the present all kind of groundwater manage model , combined mathematical programming mathematical statistics random process and the theory of variation system of groundwater resources on the unite optimum attempter of surface water and groundwater , emphasized how to make the model more nicety , more simple , more practicality ; ( 6 ) analyzed the inside condition and outside condition to assure the sustainable and optimum exploi tation of groundwater resources , the inside conditions are the follows : correct resources idea , scientific methods of resources calculation and evaluation , credible forecast methods of resources , exercisable measures of resources management , the outside conditions are the follows : the development idea of high layer , the transform of manage system , the matched policy and rule of law , the adjusted of economy lever , the improve of cultural diathesis , the boosting up of water - saving consciousness and detail measures , the control of population rising , the prevention and cure of water pollute , the renew and rebuild of ecology ; ( 7 ) scan the sustainable and optimum exploitation of groundwater resources from the high level of metagalaxy , earth system science , and philosophy ; lint out the more directions on groundwater resources
  基于以上考虑，论文主要从以下几方面对地下水资源可持续开发问题进行了比较深入的探讨：全面回顾了“可持续发展”概念的由来与演变，对国内外“可持续发展”的研究现状进行了述评，并对“可持续发展”概念的科学内涵进行了深入探讨；对涉及地下水资源的一些最基本的概念和命题进行了全面的回顾和评述，对目前仍然存在的一些错误观点和混乱认识提出了自己的见解；全面阐述了地下水资源变值系统理论的内容和意义，并与传统的地下水资源计算评价方法进行了对比分析，结合实例具体说明了方法的应用；深入分析了地下水资源预测预报工作的极端重要性和复杂性，对传统的地下水资源动态预测方法进行了全面的评述，指出了各类预测预报方法的特点及适用条件，对最近二十多年刚发展起来的小波分析技术的主要思想和方法及其应用范围，以及号称第五代计算机语言的matlab软件和附带的小波分析工具箱进行了介绍，并应用于地下水动态过程线的分析，采用时间序列中的b ? j法，蒙特卡罗方法，与地下水资源变值系统理论相结合，探讨了地下水动态资料分析和地下水资源预测预报的新思路；综合分析了现今各类地下水管理模型的特点及缺陷，将数学规划、数理统计、随机过程等与地下水变值系统理论相结合进行地表水地下水或多水源的联合优化调度，使模型更准确、更实用；对保证地下水资源可持续开发的内部条件和外部条件进行了分析，内部河海人学博卜学位论文前言、摘要、目录条件主要是正确的资源观，科学的资源计算与评价方法，可靠的资源预测预报技术，可操作的资源管理措施，外部条件主要是高层发展思路、管理体制的变革、配套的政策法规、经济杠杆的调节、人文素质的提高、节水意识的增强及具体节水措施、人口增长的控制、水体污染的防治、生态的恢复和重建等;从宇宙科学、地球系统科学及哲学的高度审视地下水资源的可持续开发;指出了地下水资源可持续开发的进一步研究方向。

• 过程线的日语：ハイドログラフ すいいず りょうすいきょくせん