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针对电提取离子法找矿工作中存在的问题,提出了一些改进建议,强调建立“参照系”采样工作的重要性,并提出以“提取系数”作为成果评价的基础. 相似文献
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从原理上讲,电提取离子法适用于任何能够形成离子晕的矿产资源和地质问题.自从电化学找矿方法(主要是其中的电提取离子法)在有关学术会议和刊物上发表后,受到了很多单位的重视.为了推广该方法用于生产,我们举办了(还将继续举办)两期短训班,对某些理论和实际问题进行了广泛地探索和讨论,现就其中的几个问题谈谈自己的认识和看法. (一)电提取离子法中电极上所提取元素的 相似文献
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本文从力学和统计物理学两个角度论证了以下结论:在电提取离子法工作中不应该统一各指示电极的电流强度,而应该统一各指示电极附近的电场强度。或者说,各指示电极的电流强度大小与指示电极上的提取量无关。 相似文献
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电提取离子法在提取离子时是一个动态过程,提取量不但与提取时间有关,而且与指示电极的位置有关。检查工作量应布置在有电提取离子法异常的地段上,把质量检查和异常检查合并。第一、二次提取的异常明显存在,相对误差在20%以内,是矿致异常;第二次撮以量大于第一次几倍或更多,显示有隐伏金矿体存在;第二次提取量比第一次稍大,相对误差大于60%,提取量的数值小于或稍高于背景值,是背景区。2次测定结果的相对误差δ≤45%为合格,一个级。对四级质量的成果应扩大到20%的检查量,若质量仍达不到要求,应在检查量所代表的范围内返工。 相似文献
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直接计算磁性下界面深度的功率谱法 总被引:1,自引:0,他引:1
以计算居里等温面深度为目的,本文给出了利用磁异常的垂向导数的功率谱来直接计算磁性下界面深度的方法。同时,借助于异常场的谱与其垂向导数谱之间的关系,还可由用磁异常垂向导数功率谱计算的公式转换出用异常场的功率谱来计算磁性体下底深度的公式。理论模型实验表明,两种计算方法均能得到较好的结果。最后给出了用该方法对泛华北地区航磁异常的试算结果。 相似文献
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电提取离子法中离子运移机理初探 总被引:1,自引:1,他引:0
首先讨论了大量离子系统的初值问题,随后介绍了6个基本概念,估算了地层中离子的平均热运动速度。导出了离子散射的指数规律,得出离子的平均自由时间的数值等于散射几率的倒数;离子的平均漂移速度和电场强度成正比,离子淌度与平均自由时间成正比,与有效质量成反比;介质的电导率和离子浓度、平均自由时间成正比,与有效质量成反比的结论有有关公式、表达式。指出了离子的运移机理是,运移-散射-再运移-再散射,直到离子被吸 相似文献
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本文介绍的找金新方法——电提取离子法,通过在已知金矿点上的试验,不仅取得了较好结果,更重要的是通过对提取电源的试验对比,证明选用微型电池(1.5V)进行提取也可获得满意结果,从而大大提高了方法的野外适用性。 相似文献
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地电化学提取法机理研究 总被引:2,自引:0,他引:2
通过系统地研究几种矿物及土壤中的铜离子在电场作用下的溶出机理及迁移规律,得出地电化学提取法中的一般规律。在激发电场作用下,土壤中矿物的成矿元素可被加速溶出,并发生难溶形态→溶解度稍大的形态→可溶形态转化。同时离子的扩散系数最大比未加电场时增大约500倍.离子的迁移速度也增大了约50倍,流量也有明显提高。地电提取法提取的元素异常主要来源于电极周围附近的土壤(及所含的矿物)中。该异常是深部矿物所形成的离子晕的结果.并且与土壤中矿物元素的化学形态有关。 相似文献
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Groundwater is the prime source in the area of Varaha River Basin, Andhra Pradesh, India. Groundwater samples collected during
pre- and post-monsoon were analyzed for major ion chemistry to understand the operating mechanism of geochemical processes
for variation of groundwater quality. Low ionic concentration is observed in the groundwater occurring at topographic-highs
and towards the river compared to the rest of the area. This is caused by the influence of recharge water. Geochemistry of
groundwater is observed to be mainly controlled by the rock-weathering, mineral dissolution, leaching, ion exchange and evaporation,
and is subsequently modified by the anthropogenic and marine activities. Contribution of residual soluble salts below the
depth of 5 m from the ground surface is high, while it is low beyond the depth of 5 m. Anthropogenic activities cause an accumulation
of excess residual soluble salts in the former depth and the content of this soluble matter is reduced by the clay products
beyond the latter depth. Seasonal ionic concentration of groundwater is greatly influenced by the recharge process with reference
to topographical features, lithological characteristics and anthropogenic activities. Groundwater quality is classified as
mixed and non-carbonate alkali groups due to a combined action of geogenic/anthropogenic and marine sources, respectively.
The groundwater quality is above the adequacy level for both drinking and irrigation, and appropriate management measures
are recommended for sustainable development. 相似文献
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经典的Prandtl 机构不能很好地反映支护结构入土深度的影响,也不能反映土体强度非均质和各向异性的影响。根据塑性极限分析上限定理,基于修正的Prandtl机构,推导了既可以合理反映支护结构入土深度影响,又可以反映土体强度非均质和各向异性特性的基坑抗隆起稳定的上限解公式,同时基于商业化程序的二次开发,建立了可以考虑土体强度非均质和各向异性影响的强度折减弹塑性有限元方法。通过提出的修正Prandtl机构上限解与强度折减有限元方法以及多块体上限解的对比,验证了修正机构上限解以及强度折减有限元法的合理性和可行性,最后讨论了非均质系数、各向异性系数、支护机构入土深度等因素对基坑抗隆起稳定性的影响,并通过了实例的验证,相关结论可供工程参考。 相似文献
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基于孔隙承压水属性,研究了苏锡常地区孔隙Ⅱ承压水超采状态下最大水位埋深期(1994年、1998年)地下水动态(水位、水质)监测资料与水文地质条件。论述水位动态虽能直观反映开采状态下水资源衰竭与水位变化特征,但对补给条件及水动力机制不清楚,则会给超采状态下水文地质条件认识及评价带来视觉上的偏颇。采用水化学动力参数则能很好地反映不同水源补给空间的变化规律,用其常量水化学组分(K+、Na+、Ca2+、Mg2+、Cl-、HCO-3、CO2-3、SO2-4)计算的离子强度(I)、主要离子活度(aHCO-3、aNa+ 相似文献
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Ionic liquid as a medium to remove iron and other metal ions: a case study of the North Kelantan Aquifer,Malaysia 总被引:1,自引:1,他引:0
Nur Hayati Hussin Ismail Yusoff Yatimah Alias Sharifah Mohamad Nurul Yani Rahim Muhammad Aqeel Ashraf 《Environmental Earth Sciences》2014,71(5):2105-2113
An alternative iron removal treatment method using liquid-liquid extraction with the room-temperature ionic liquid, 1-butyl-3-methylimidazolium bis(trifluoromethanesulfonyl)imide, as a solvent medium was studied. The chelating agent 1,10-phenanthroline was used as the extractant. The extraction of Fe(III) and Fe(II) was influenced significantly by the pH of the aqueous phase. The successful removal of iron was achieved; more than 95 % of the initial iron concentration was removed from the groundwater samples. However, detailed research is needed before the ionic liquid method can replace the conventional groundwater treatment protocol because the recovery rate was very low upon reuse (approximately 25–60 %). This low recovery was due to the ion exchange process; the appearance of anions from ionic liquids was also detected in groundwater samples. 相似文献
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An experimental survey of the gold concentrated from well water by a hydroelectrical extraction (HEE) method has been carried out in the famous Au metallogenic province in the eastern part of Shandong Province in northeastern China. This method is based on the existence of ionic Au in groundwater around ore bodies. Under the action of an external electric field, ionic Au migrates toward the cathode where the metal is absorbed by a special absorbent attached to the cathode. Promising areas for further exploration can be evaluated from the amount of Au in the absorbent.Distinct Au anomalies were discovered by the experimental survey. The results from the follow-up study of some of these anomalies have shown that most of them are related to the known placer Au deposits and to the primary Au occurrences. However, two new Au prospects and several new Au sources have been found which offer new targets for Au hunting in the area.The hydroelectrical extraction method is an effective technique of looking for Au in areas covered with transported overburden. Since the Au in well water can be concentrated on the cathode with the absorbent, the sensitivity requirement for Au analysis could be reduced. The method also provides a useful tool for the exploration of blind placer Au. 相似文献