助手标题  
全文文献 工具书 数字 学术定义 翻译助手 学术趋势 更多
查询帮助
意见反馈
   长石水解 的翻译结果: 查询用时:0.184秒
图标索引 在分类学科中查询
所有学科
地质学
更多类别查询

图标索引 历史查询
 

长石水解
相关语句
  相似匹配句对
     Hydrolysis of Waste Paper
     废纸的水解
短句来源
     HYDROLYSIS OF POLYACRYLAMIDE AND ITS COPOLYMERS
     聚丙烯酰胺的水解
短句来源
     EXPERIMENTAL RESEARCH ON DE-IRONING OF FELDSPAR
     长石除铁试验研究
短句来源
     Summarization of comprehensive utilization of potash feldspar
     钾长石综合利用综述
短句来源
查询“长石水解”译词为用户自定义的双语例句

    我想查看译文中含有:的双语例句
例句
没有找到相关例句


The ore-bearing rock of the Xiaowenshan detrital mica mineral is a set metamorphic rock that main body rock is muscovite K-feldspar gneiss. The protolith is clayey sandstone that high in Si,K and low in Ca,Mg. Genesis of the detrital mica mineral mianly was effect of migmatization with K-replacement. In the migmatization the hydrometosomatismof k-feldspar lead to formation and concentration of detrital mica mineral. The ore-forming proces underwent two stage of early and later, which result in the detrital mica...

The ore-bearing rock of the Xiaowenshan detrital mica mineral is a set metamorphic rock that main body rock is muscovite K-feldspar gneiss. The protolith is clayey sandstone that high in Si,K and low in Ca,Mg. Genesis of the detrital mica mineral mianly was effect of migmatization with K-replacement. In the migmatization the hydrometosomatismof k-feldspar lead to formation and concentration of detrital mica mineral. The ore-forming proces underwent two stage of early and later, which result in the detrital mica bodys with variety of ore type,lamell asize, Scale.

小文山碎云母矿的含矿岩石是一套以白云母钾长片麻岩为主体的变质岩,原岩为富硅高钾、低钙低镁的粘土质砂岩。碎云母矿的形成主要受晚期以钾质交代为主的混合岩化作用的影响,混合岩化过程中钾长石的水解作用导致碎云母矿的形成和富集。成矿作用主要经历早、晚两期,形成了矿石类型各异、片度、规模大小不同的碎云母矿体。

Crevice water in the Panshan granite originates from meteoric water. It occurs in fissures of various origins. The age of crevice water is very different, varying from less than 4 years old to about 40 years old. The common elements and trace elements in crevice water are mainly derived from hydrolysis of feldspars, especially anorthite. The contents of SiO2 and Sr in crevice water are relatively high and have met the standards of drinking mineral water. The amount of minable crevice water resources is 12. 9156...

Crevice water in the Panshan granite originates from meteoric water. It occurs in fissures of various origins. The age of crevice water is very different, varying from less than 4 years old to about 40 years old. The common elements and trace elements in crevice water are mainly derived from hydrolysis of feldspars, especially anorthite. The contents of SiO2 and Sr in crevice water are relatively high and have met the standards of drinking mineral water. The amount of minable crevice water resources is 12. 9156 million m3/a on average. The regularity of crevice water yield is clear.

盘山花岗岩裂隙水起源于大气降水,赋存于各种成因的裂隙中,裂隙水年龄从小于4a到接近40a,差异较大。裂隙水中常量元素和微量元素主要来源于长石类矿物的水解,特别是钙长石的水解,其中SiO_2和Sr在裂隙水中含量较高,已达到饮用矿泉水标准。裂隙水可开采资源量多年平均为1291.56万m~3/a,富水规律明显。

The hydro-chemical characteristics of stream flow within the headwater drainage of the rümqi River, Tianshan Mountains, is affected by various factors, such as precipitation, glaciation, snow melting, permafrost active layer, moraine components and talus-soil-water interaction in warm season. The wide meltwater-soil interaction and chemical denudation of mineral solutes dramatically contribute to the stream water, resulting in higher solute concentration in stream water than that in precipitation. Pyrite oxidation,...

The hydro-chemical characteristics of stream flow within the headwater drainage of the rümqi River, Tianshan Mountains, is affected by various factors, such as precipitation, glaciation, snow melting, permafrost active layer, moraine components and talus-soil-water interaction in warm season. The wide meltwater-soil interaction and chemical denudation of mineral solutes dramatically contribute to the stream water, resulting in higher solute concentration in stream water than that in precipitation. Pyrite oxidation, calcite dissolution and K-feldspar hydrolyze are the main reactions, causing high Ca 2+, K +, SO+ 2- 4 concentrations and weak alkaline pH value in stream water. Ca 2+, Mg 2+, SO+ 2- 4 and K + concentrations with their ionic pulse peaks in the Glacier No. 1 are much higher than those in the Dry Cirque and the Total Control Gauge Section due to more effective snow melting and glacier grinding on the underlain rocks that boosts mineral dissolution. Stream flow in the Dry Cirque is more influenced by precipitation, except for soil-restored meltwater mixing and soil-water interaction. The Total Control Gauge Section generally shows a mixed effect of the Glacier No.1 and the Dry Cirque.

天山乌鲁木齐河源暖季径流水文化学特征受大气降水、冰川作用、积雪消融、冻土活动层状况以及水岩相互作用等因素综合影响 ,普遍存在的水岩相互作用和冰碛物岩矿离子组分的化学剥蚀作用导致径流中各项离子浓度远远高于大气降水中相应值的规律 ,其中黄铁矿氧化反应、钾长石水解和方解石水解反应为控制流域径流偏碱性的主要化学作用 .冰川磨蚀对于岩矿溶解的增强作用和相对更强的积雪消融导致天山乌鲁木齐河源 1号冰川径流的Ca2 + 、Mg2 + 、SO2 -4 和K+ 离子浓度和离子脉冲峰值远高于空冰斗和总控水文点 .空冰斗融水径流受大气降水、季节性冻土活动层融水混入以及融雪水与土壤相互作用影响更大 ,表现出更显著的Cl-、Na+ 和NO-3 离子峰值现象 .总控水文点则大体上反映上述二水文点的混合作用 ,变化相对平缓 ,离子浓度峰值介于二者之间 .

 
图标索引 相关查询

 


 
CNKI小工具
在英文学术搜索中查有关长石水解的内容
在知识搜索中查有关长石水解的内容
在数字搜索中查有关长石水解的内容
在概念知识元中查有关长石水解的内容
在学术趋势中查有关长石水解的内容
 
 

CNKI主页设CNKI翻译助手为主页 | 收藏CNKI翻译助手 | 广告服务 | 英文学术搜索
版权图标  2008 CNKI-中国知网
京ICP证040431号 互联网出版许可证 新出网证(京)字008号
北京市公安局海淀分局 备案号:110 1081725
版权图标 2008中国知网(cnki) 中国学术期刊(光盘版)电子杂志社