盐湖

The characteristics and development status of salt lake resources in Chadamu basin were analyzed.

概述了青海盐湖矿产资源状况，重点分析了柴达木盆地盐湖资源的特点和开发现状，阐述了盐湖资源开发中存在的问题，提出了盐湖矿产资源实施可持续发展战略的对策与措施。

In traditional classification, saline lake study was part of limnology that studied the physics, chemistry and biology of lakes W.

盐湖学的基本任务是用多学科的原理为指导，系统地研究与勘查盐湖，为人类与盐湖的协调及其科学管理和合理利用提供科学技术依据，为持续发展"盐湖农业"、盐湖矿业和旅游业服务。

In this paper,by considering the characteristics of magnesium resources in salt lakes in China,the research progress in the preparation and utilization of magnesium hydroxide,magnesium oxide,magnesium metal and alloys,magnesium oxychloride cements,and ...

本文针对我国盐湖镁资源的特点，综述了和盐湖镁资源开发利用相关的氢氧化镁、氧化镁、金属镁、镁合金、氯氧镁水泥和镁质晶须的开发及研究进展，并对我国盐湖镁资源的开发利用提出了一些建议。

Now 24 Salt Lake, mainly Chaerhan Salt Lake, tea cards Salt Lake, hoh Salt Lake, quint according to Salt Lake and so on, the average thickness of salt layers 4 to 8 meters, 60 meters thick, believed to be rich in salts and other chemicals element.

现在又24个盐湖，主要有察尔汗盐湖、茶卡盐湖、柯柯盐湖、昆特依盐湖等，盐层平均厚4～8米，最厚60米，蕴藏有丰富的盐类和其他化学元素。

Aimed at salt lakes in Qaidam, the qualitative and quantitative simulationwe made can further enrich and develop the theory of mixture about the formation and evolution of salt lakes. Some results we obtained can be theoretically used to choose and establish technological processes of a salt pan for exploiting K resource of MgSO4 sub-type salt lakes in Qaidam Basin.

针对柴达木盆地盐湖，从定性或定量模拟研究的角度，我们的研究丰富和发展了盐湖形成演化过程中的混合掺杂作用理论，某些研究成果可以用于柴达木盆地硫酸镁亚型盐湖钾资源开发前期选取和进行工艺路线设计的理论预判断上。

Using the sign if icance of these characters in the aspect of sediment environment, th is paper analyzed C and O iso tope ofQ ian jiang Saline lake and educed conclu sion s: there are good relat ivity betw een the change of clim ate and sedim ent\r\nenvironm en t and the con tent's change of C and O iso tope from high to low; it is aobturated saline lake of\r\ninnerland tow ard Q ian jiang saline lake, and the con ten t of C and O iso tope was primarily decided that Ciso tope is - 5‰ and O isotope is - 2‰.

主要介绍了碳和氧同位素的地球化学特征，利用这些特征在沉积环境方面的指示意义分析了潜江盐湖的碳、氧同位素并得出了以下认识：碳、氧同位素值的高低变化与气候的变化和沉积环境的变化具有很好的相关性；潜江盐湖是一个封闭的内陆盐湖，就该湖而言，其碳同位素值可初步确定为- 5‰，其氧同位素值为- 2‰。

The reason of the form of salt lake is disaster and the movement of the earth's crust,Qinghai-Tibet plateau was one part of ocean in the past,by long-term movement of the earth's crust,the surface was raise to be the biggest plateau in the world,as a result,seawater had been left in some bottomland then forming salt lakes and ponds,Chaka Salt Lake was one of them.

盐湖的形成是由于灾难或地壳运动，青藏高原从前是海洋的一部分，经过长期的地壳运动，这块地面抬起变成了世界上最大的高原，结果海水留在了一些低洼地带形成了许多盐湖和池塘，茶卡盐湖就是其中一个。

Chaka Salt Lake Chaka Salt Lake:Chaka means"Salt lake"in Mongolian. The area is about more than 100 kilometers.

6《茶卡盐湖》茶卡盐湖：茶卡是蒙古语，意为&盐湖&，面积约 100多平方公里。

About the formation of salt lakes in Qaidam Basin, We respectively simulated and studied the relation between the formation of salt lakes and the origin of waters in Chaka Salt Lake distributed in the Small basin on the south of Qilan mountain and all salt lakes distributed in Big basin.

对于柴达木盆地盐湖的形成，分别模拟研究了柴达木盆地祁连山南缘山间小盆地内分布的茶卡盐湖和大盆地范围内各盐湖的形成同水体来源的关系。

Field investigations on reinforced concrete structures in Qinghai salt lake region discovered that corrosions of concrete and steel reinforced concrete were particularly serious and universal.

第二章简要介绍了我国盐湖地区的环境气候条件，针对典型盐湖卤水中含有的对混凝土产生物理化学腐蚀的侵蚀性离子浓度，重新划分了盐湖卤水的类型，现场考察了混凝土与钢筋混凝土结构在青海盐湖地区的腐蚀与破坏现状。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。