成矿流体来源主要为大气降水。
Metallogenetic epoch was late Yanshanian and fluid derived from meteoric water.
大气降水是本区植物繁衍的主要补给源。
The precipitation isa main replenishment sources for plant growth in this area.
认为该矿床主要由大气降水的环流形成。
It is concluded that Zjinshan deposit formed mainly by the convective circulation of meteoric water.
大气降水淋滤-渗滤模式。
半于旱地区的沙漠地带，大气降水基本全部入渗。
In the area of semi - arid desert, the precipitation almost seep completely.
同位素和包体资料表明成矿溶液主要为大气降水。
Meanwhile, the isotopic and inclusion data show that mineralizing solution is mainly meteoric water.
阐述了成矿溶液中的水主要来自大气降水的事实；
地下水起源于大气降水，但雨水的下渗速度极为缓慢。
The groundwater originates from the precipitation, but it infiltrates very slowly.
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.
各植被类型的土壤含水量与大气降水具有相似的季节动态；
The soil water change in all kinds of vegetation types is consistent with seasonal rule of Precipitation.
该网站提供了美国200多大气降水化学性质监测站的数据。
The NADP home page offers data from a US network of 200 precipitation chemistry and atmospheric monitoring stations.
雨量是大气降水的量度，还是人工增雨效果评估的重要参量。
Rainfall amount is used to measure precipitation and also to evaluate the precipitation enhancement effect as an important parameter.
分析了新疆43号泉水流量的地震前兆特征及大气降水影响。
Seismic precursor characteristics of the spring no. 43 in Xinjiang and the rainfall influence on it are analysed in the paper.
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。
Soil water movement is mainly influenced by site type, vegetation and atmosphere precipitation.
天B池水色碧蓝，澄清，靠大气降水和地下水补给，水位变化小。
Days B water color blue, clarify, by atmospheric precipitation and underground water supply, water level fluctuations.
WSR- 88d级的雷达系统有很多适用于生成大气降水数据的采集模式。
The WSR-88D class radar systems have many acquisition modes for developing data on atmospheric precipitation.
采用D、18O同位素峰值位移法求出研究区大气降水入渗补给量。
The D, 18O isotopes peak displacement method is used to estimate the precipitation infiltration quantity in the study area.
西北荒漠化地区，包气带中的水分除来自大气降水外，还来自凝结水。
In desertification areas of northwest China, the water content in the unsaturated zone originates from atmospheric precipitation and from water condensation.
土壤碳的这种分布格局与大气降水的淋溶、土壤生物活动等因素有关。
This distribution pattern of soil carbon was related to such factors as the precipitation eluviation and the organism activities in soils.
地热田油同位素研究证明：蒸气井热流体的95左右是大气降水成因的。
Isotopic studies from geothermal fields indicate that about 95% of the thermal fluid from steam Wells is meteoric in origin.
地热田油同位素研究证明：蒸气井热流体的95%左右是大气降水成因的。
Isotopic studies from geothermal fields indicate that about 95% of the thermal fluid from steam Wells is meteoric in origin.
会泽铅锌矿床的成矿模式可概括为“大气降水淋滤-对流循环-富集成矿”。
The ore-forming pattern can be generalized "atmosphere water leaching -convection circle -metallogenic".
氢氧同位素数据在大气降水线附近，指示了晚阶段大气降水参与的积极影响。
Hydrogen and oxygen isotope data line in the vicinity of the meteoric water line, indicating meteoric water's enrollment at the late stage.
通过氧同位素研究证明了成矿溶液的来源由早期岩浆水转变为晚期大气降水；
The isotopic composition of oxygen shows that the origin of the ore forming solution was turn from magmatic water in early stage to circulated meteoric water in later stage.
结果表明，向斜核部的深部承压水，同时接受向斜东翼和西翼大气降水的补给。
The result shows that the deep confined karst water is supplied by the water from both the east wing and the west wing of Maoba syncline.
稳定同位素特征揭示了矿质来说从围岩中淋取；成矿溶液主要来源于大气降水。
The characteristics of stable isotope indicatedthat the ore-forming material was leached from the wall rocks ; and the ore-forming fluid wasmainly supplied by meteoric water.
渗入水由大气降水和地表水的渗入产生，受重力作用由盆地边缘向盆地中心呈向心流。
While infiltration water generated from filtration of meteoric water and surface water flows from basin edge to its center in gravity -induced centripetal flow.
各林分地表径流的总磷、总氮含量均高于大气降水，樟落混交林的总磷、总氮含量最高。
The content of total nitrogen and total phosphorus in every forest runoff is higher than rainfall, and that of Coniferous mixed forest is the highest.
应用大气降水中的氚做示踪核素来研究地下水的运动状态，必然遇到氚的输入背景值问题。
In the study of groundwater movement using tritium in atmospheric precipitation as tracer, we will inevitably encounter the input background value problem of tritium.
应用大气降水中的氚做示踪核素来研究地下水的运动状态，必然遇到氚的输入背景值问题。
In the study of groundwater movement using tritium in atmospheric precipitation as tracer, we will inevitably encounter the input background value problem of tritium.
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