大气水

3mm波段地面遥感大气水的研究

Research on Remote Sensing of Atmospheric Water by Means of Ground Based 3 mm Band Radiometry

微波遥感大气水的研究

Research on Microwave Remote Sensing of Atmospheric Water

对超高压变质岩中O、C、H等同位素的研究进一步表明，超高压变质作用过程中并无大规模流体活动，大气水的O同位素成分可被带到地幔深处而不改变；

Fluids were not active and oxygen isotope composition of meteoric water could be preserved during UHPM process , as is evidenced by O , C , and H isotope data ;

秋季净光合速率呈双峰曲线，影响光合速率的主要因子为光合有效辐射、蒸腾速率、胞间CO2浓度和大气水气压亏缺；

The photosynthetic rate showed a double-peak curve in autumn , the major factors affecting the photosynthetic rate were E , PAR , Ci and VPDL .

酶催化荧光法测定大气水相中过氧化氢

Determination of hydrogen peroxide in atmospheric precipitation by enzyme catalyzed fluorometric method

大气水偏摩尔焓>土壤水偏摩尔焓>植物水偏摩尔焓。

Soil water > plant water > atmospheric water .

大气水腿管在真空洗浆机上的应用

The Application of Barometric Leg in Vacuum Filters

大气水地表水土壤水地下水相互转化关系的试验研究

Experimental research on the mutual transformation relationship between meteoric water soil water and ground water

影响储层发育的因素有岩石类型、沉积微相、成岩作用及大气水埋藏成岩作用。

The controlling factors of reservoir development such as rock type , sedimentary facies and diagenesis .

台北凹陷地下水动力场模式属不对称型：凹陷北部边缘地区为大气水下渗形成的向心流；

For the Taibei depression , the hydrodynamics in the Jurassic reservoir is characterized by asymmetry .

矿床氢同位素值低是由于岩浆热液与大气水混合形成。

The low value of hydrogen isotope may caused by the mixing of magmatic hydrothermal and rain-water .

大气水－砂岩的相互作用是盆地流体研究的重要内容。

The interaction of meteoric water-sandstone is an important part of the research of the basin fluid .

大气水-砂岩的相互作用

The Interaction of Meteoric Water-Sandstone

古大气水淋滤作用是改善不整合面附近储层物性的重要因素。

The ancient meteoric water eluviation is the important way to improve reservoir physical properties under the unconformity .

流体不混溶、水－岩反应及古大气水的混入是造成本区金沉淀成矿的主要因素。

Fluid immiscibility and fluid rock interaction may be the main causes for gold deposition in the mine .

氧同位素会随着大气水循环而变化，硫同位素则根据地球岩床的不同而变化，通过它们我们就能确定地理位置。

Oxygen isotopes vary with the water cycle , and sulfur with bedrock , so they 're location proxies .

西太平洋暖池和北京地区大气水特征的地基遥感测量

Characteristics of Atmospheric Water over Western Pacific Warm Pool and Beijing : A Summary of Ground-Based Microwave Radiometric Measurements

后期可细致分析此次降水过程中的大气水平衡及水分收支转换和云水资源量。

The atmospheric water balance , moisture budget and cloud water resource of this event can be analyzed later .

所有这些，在很大程度上取决于空中水资源和大气水循环的变化及其趋势。

All these results depend largely on the changes and the trends of the air water resource and atmospheric water cycle .

其中大气水淋滤形成的次生孔隙对异常高孔隙的贡献较小。

Among them , leaching of meteoric water has contributed less to the formation of anomalously high porosity zones compared to other factors .

初始的成矿流体是一个低盐度的以H2O－NaCl-CO2为主的上学体系，主要源于大气水与变质建造水的混合。

The primary mineralizing fluid is a H2O-NaCl-CO2-dominated system with low salinity , principally derived from a mixed source of metamorphic and meteoric water .

论文主要取得的成果认识如下：（1）金湖凹陷西斜坡外坡带受大气水下渗影响作用强，地层水矿化度低。

The results in the research as follows : ( 1 ) Influenced by meteoric water strongly , the salinity of formation water is low .

由于角砾岩体的隐爆、流体减压沸腾及古大气水的混入，热液中的金被沉淀成矿，形成胶结物型和脉型金矿化。

Cryptical blasting , fluid boiling and meteoric water mixing are reasons of gold deposition in the deposit , forming cement type and vein type mineralisation .

成矿流体主要为变质变形过程中产生的变质热流体、再循环大气水和地球深部的高温、高压流体。

The ore-forming fluid consists mainly of metamorphic fluid , recycled atmospheric water and high-temperature and high-pressure fluid from deep earth during the process of metamorphism-transformation .

古表生期大气水溶蚀作用扩大了储层分布范围、发育规模和提高了储层质量；

The dissolution of atmospheric water in ancient epigenenesis expanded the distribution of reservoir and the scope of the development scale and improved the quality of reservoir .

矿物流体包裹体成分反映了两种不同性质热液的活动，氢、氧同位素组成所指示的成矿热水以大气水或地下热卤水为主。

Hydrogen and oxygen isotope composition of water in fluid inclusions indicates that ore - bearing hydrothermal solution origined mainly from atmospheric water or deep connate water .

玢岩铁矿成矿温度介于两者之间。从低硫亚类浅成热液矿床、高硫亚类浅成热液矿床到斑岩型矿床，流体中大气水含量逐渐减少，岩浆水含量逐渐增多。

From low-sulfidation epithermal depostis , high-sulfidation epithermal depostis to porphyry deposits , the meteoric water content decreased and the magmatic water content increased in the ore-forming fluids .

冷却地层水对碳酸盐矿物的溶解形成孔隙等。这些孔隙的形成机制特别是新提出的大气水的溶解作用对于次生孔隙成因的解释和地下岩石孔隙的预测意义十分重要。

It is important to understand these mechanisms such as dissolution of sediment by the meteoric water especially for interpretation of secondary porosity and prediction of subsurface porosity .

通过方解石脉稳定碳氧同位素和包裹体均一温度测定，恢复了黔南桂中坳陷海相地层古大气水下渗深度。

Through the analysis of stable carbon and oxygen isotopes of calcite veins and homogenization temperature of fluid inclusion , the ancient meteoric water infiltration depth was recovered .

由于构造运动，裂隙发育，后期富矿热液向上运移，并在适当条件充填成矿，后期与大气水混合成矿。

Fissure developed as tectonic movement , late stage hydrothermal of ore-rich migrate upward , and mineralization by filling in the appropriate condition , later mineralization mixed with rain-water .