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budget
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  预算
     Study on the Expenditure Budget Management in Shipping Support System
     航运支持系统的支出预算管理研究
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     Study on the Strategy-oriented Enterprises Comprehensive Budget Management System
     基于战略导向的企业全面预算管理体系研究
短句来源
     Application of Microcomputer in Engineering Budget
     微机在工程预算中的应用
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     The Data Files Design of Budget Program
     工程预算软件定额数据文件设计
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     NATIONAL BUDGET AND FISCAL POLICY IN INDIA
     巴基斯坦国家预算和财政政策
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  收支
     Energy budget equation was determined under satiation condition:100C=64.5R+20.7G+10.6F+4.2U.
     h. 得到了在饱食状态下的能量收支方程:100C=64.5R+20.7G+10.6F+4.2U.
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     The study was conducted to investigate the effects of sodium chloride as a diet supplement(0,0.05%,0.10%,0.20%,0.40%,0.80%,1.60%,3.20%,6.40% and 12.80%) on the survival,growth and energy budget of Litopenaeus vannamei juvenile with the initial wet body weight of 1.041g~1.104 g.
     研究了饲料中添加氯化钠(0,0.05%,0.10%,0.20%,0.40%,0.80%,1.60%,3.20%,6.40%和12.80%)对体湿质量为1.041~1.104g凡纳滨对虾(Litopenaeusvannamei)的存活、生长和能量收支的影响。
短句来源
     The experiment was conducted to determine the effects of stocking densities (12.04, 24.08, 48.16, 144.49, 240.81, 337.13, 433.46, 529.78, 626.11 individuals/m2) on survival, growth and energy budget of juvenile L. vannamei with the initial wet body weight of (0.026±0.006)g.
     研究了密度(12.04、24.08、48.16、144.49、240.81、337.13、433.46、529.78、626.11尾/m2)对凡纳滨对虾(平均初始湿重0.026±0.006g)存活、生长和能量收支的影响。
短句来源
     The equation of energy budget is C=G+R+U+F,in it,R=SDA+R_S+R_A;
     能量收支方程为:C=G+R+U+F,其中,R=SDA+RS+RA;
短句来源
     The energy budget model can be written as: 100 A =30 37 R +69 63 G and 100 A =48 89 R +51 13 G at the density of 5 kg/m 3 and 8 kg/m 3 respectively.
     黑在密度为 5 kg/m3和 8kg/m3下的能量收支模型分别为 :1 0 0 A=3 0 .3 7R+69.63 G和 1 0 0 A=48.89R+5 1 .1 3 G。
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  “budget”译为未确定词的双语例句
     A SEDIMENT BUDGET EQUATION AND IT'S APPLICATION IN ESTUARY
     河口沙量平衡方程及其应用
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     THE WATER VAPOUR CONTENT AND THE WATER BUDGET IN THE ATMOSPHERE OVER CHINA
     我国大气中平均水汽含量与水分平衡的特征
短句来源
     AN ANALYSIS OF FIELD-WATER BUDGET OF THE MAIN CROPS ON THE LOW PLAIN IN HEBEI PROVINCE
     河北省低平原地区主要作物农田水分盈亏分析
短句来源
     THE BUDGET EQUATION OF ENERGY POTENTIAL VORTICITY AND ITS APPLICATION TO DIAGNOSIS OF HEAVY RAIN
     能量位涡度平衡方程及其在暴雨诊断分析中的应用
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     Fuzzy Represention of Firm's Demands Under the Soft Budget Constraints
     软约束下企业需求的模糊表示
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  budget
Due to the uneven distribution of rainfall, the water budget balance was slightly affected in May and November.
      
They play a crucial role in preventing soil erosion and conserving large amounts of water thereby regulating the water budget of local ecosystems.
      
Time budget and activity rhythm of wild Great Bustard in winter
      
Instantaneous scanning and focal animal sampling methods were used to record the behaviors of nine wild Great Bustards (Otis tarda) and their time budget from November 2004 to January 2005.
      
Non-parameter testing demonstrates that time budget among resting, flying and others in two temperature intervals (>amp;gt; -5 °C and ? -5 °C) was significantly different.
      
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This paper is the first part of research concerning the budget of the atmospheric radiation energy over Eastern Asia. We have discussed following three problems:1.From the experimental values for each band of the absorption spectra of water vapor a formula (6) suitable for hand computation of the absorption of solar radiation, is obtained. It is compared with Mugge-Moller formula.2.By formula (6), the absorption energy of solar radiation and heating rate from the surface to 100 mb were computed for January...

This paper is the first part of research concerning the budget of the atmospheric radiation energy over Eastern Asia. We have discussed following three problems:1.From the experimental values for each band of the absorption spectra of water vapor a formula (6) suitable for hand computation of the absorption of solar radiation, is obtained. It is compared with Mugge-Moller formula.2.By formula (6), the absorption energy of solar radiation and heating rate from the surface to 100 mb were computed for January and July for 39 station over Eastern Asia. By considering the cloud correction, the absorption of the surface reflection of the radiation by the atmosphere, the distribution of absorption energy of the tropospheric atmosphere over Eastern Asia was obtained.3.Utilizing the data of the surface total radiation and reflection in China during 1958-1960 and the atmospheric absorption energy computed in this paper we have discussed the distribution of planetary albedo in China and the budget of solar radiation energy of the Earth and the atmosphere.

本文是讨论东亚地区大气辐射能收支研究工作的第一部分,讨论了以下三个问题: (1)本文利用文献[1]的水汽各吸收带的吸收光谱实验资料,求得了一个适合于手算的水汽对太阳辐射的总吸收能量公式(公式(6))。并把式(6)与Mugge—Moller公式进行了比较。 (2)利用公式(6),计算了东亚地区39个测站1,7月自地面到100毫巴各气层对太阳辐射的吸收能量,及其对大气的加温率。本文还进一步考虑了云的订正、大气对地面反射辐射的吸收,而求得了东亚地区对流层大气吸收能量的分布。 (3)利用1958—1960年中国地区的一些地面总辐射和反射率观测资料,以及本文计算的大气中各种吸牧能量,讨论了中国地区行星反射率的分布和地球大气系统中各种太阳辐射能的收支。

This paper is the second part of research concerning the budget of the atmospheric radiation energy over eastern Asia. We have discussed following problems:(1)The utility of Elsasser's radiation tables and its application to the construction of radiation charts.(2)The computation of the budget of atmospheric long-wave radiation and the distribution of cooling rate of the long-wave radiation for various layers for 36 stations over eastern Asia.(3)The atmospheric radiation balance and the net radiation...

This paper is the second part of research concerning the budget of the atmospheric radiation energy over eastern Asia. We have discussed following problems:(1)The utility of Elsasser's radiation tables and its application to the construction of radiation charts.(2)The computation of the budget of atmospheric long-wave radiation and the distribution of cooling rate of the long-wave radiation for various layers for 36 stations over eastern Asia.(3)The atmospheric radiation balance and the net radiation cooling rate in tropo-spheric layers.

本文系讨论东亚地区大气辐射能收支的第二部分,共讨论了以下几个问题: 1.Elsasser辐射图解资料的应用及其资料的可靠性; 2.计算了东亚地区36个站的各气层大气长波辐射的收支及长波辐射冷却率分布; 3.对流层内各层大气的辐射差额及其辐射冷却率。

This paper is the third part of research concerning the budget of the atmospheric radiation energy over eastern Asia. We have discussed following problems in this part:1.The distribution of long wave radiation and radiative balance in a cloudy atmosphere are computed. The results indicate that, except over the Tibetan Plateau for July, the features of distribution of long wave radiation in a cloudy atmosphere are similar to those in clear atmosphere both in July and January, and that the features of the...

This paper is the third part of research concerning the budget of the atmospheric radiation energy over eastern Asia. We have discussed following problems in this part:1.The distribution of long wave radiation and radiative balance in a cloudy atmosphere are computed. The results indicate that, except over the Tibetan Plateau for July, the features of distribution of long wave radiation in a cloudy atmosphere are similar to those in clear atmosphere both in July and January, and that the features of the distribution of radiative balance and distribution of long wave radiation are fundamentally the same.2.The computation of the distribution of trotospheric heat source and heat sink are carried out for eastern Asia. It is found that, the whole region is a heat sink in January and a heat source in July.3.Finally, the computation of various kinds of heat budget of the earth-atmosphere system in the various regions over eastern Asia is made. As regards to the earth-atmosphere system as a whole over eastern Asia, the heat obtained in July compensates approximately the lost in January. But only for atmosphere as a whole the heat lost is larger than heat obtained. The features of different kinds of heat budgets in different regions are different.

本文是东亚地区大气辐射能收支”的第三部分,讨论了如下几个问题: 1.云天大气长波辐射和辐射差额分布。结果指出,除7月份西藏高原地区外,云天和晴天长波辐射分布特征基本相同,而其辐射差额分布又和相应月份的大气长波辐射分布特征基本一致。 2.东亚地区对流层大气热源热汇分布:8月份整个东亚地区都是冷源,在新疆地区和中国东部北纬32°—25°之间有两个冷中心。在7月份整个东亚地区都是热源,在西藏高原东南部有一个最强的热源中心。新疆北部有一个小的热源中心。 3.东亚各地区的地气系统各种热量收支。首先就整个东亚地区地气系统而言,7月份得到热量基本上补偿了1月份损失的热量,但就大气而言,1月份热量损失大于7月份热量的获得。其次各地区各种热量收支特征并不一致。

 
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