Bromine in Oil-Field Waters and Its Use in Determining Possibilities of Origin of These Waters
Bromine in Oil-Field Waters and Its Use in Determining Possibilities of Origin of These Waters
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DOI：
10.1306/5d25c27d-16c1-11d7-8645000102c1865d
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发表时间：
1967-12
期刊：
影响因子：
3.5
通讯作者：
Gordon Rittenhouse
中科院分区：
文献类型：
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作者：
Gordon Rittenhouse
油田沃茨根据其溴含量至少可分为五组：第一组，其中溴和总溶解固体含量接近于简单浓缩海水或用总溶解固体和溴含量低的水稀释海水所预期的含量。第II组，其类似于第I组，除了对于指定的总溶解固体含量具有稍微更多至约两倍的溴。额外的溴可能是在早期成岩作用期间加入的。第III类，其中总溶解固体含量大于海水，但溴含量小于海水简单浓缩所预期的含量。这些沃茨似乎溶解了岩盐。第IV组，其中总溶解固体含量低于海水，但溴含量低于用总固体含量和溴含量低的水简单稀释海水所预期的含量。这些沃茨可以用具有可观的溶解固体但溴含量低的水稀释，或者可以是用总溶解固体和溴含量低的水稀释的III类沃茨。第V组，由溴含量高于第II组的高盐度沃茨组成。其中一些沃茨与厚盐层有关，似乎是盐层沉积后留下的蚀变苦咸水。其中一些沃茨的起源尚不清楚。
Oil-field waters can be subdivided into at least five groups on the basis of their bromine content: Group I, in which the bromine and total-dissolved-solids content approximates that to be expected from simple concentration of seawater or its dilution with water of low total-dissolved-solids and bromine content. Group II, which is similar to Group I except for having somewhat more to about twice as much bromine for a specified total-dissolved-solids content. The additional bromine may have been added during early diagenesis. Group III, in which the total-dissolved-solids content is greater than that of seawater but the bromine content is less than would be expected from simple concentration of seawater. These waters appear to have dissolved halite. Group IV, in which the total-dissolved-solids content is less than that of seawater but the bromine content is less than would be expected from simple dilution of seawater with water of low total-solids and bromine content. These waters may have been diluted with water having appreciable dissolved solids but low bromine content, or may have been Group III waters diluted with water of low total-dissolved-solids and bromine content. Group V, which is composed of high-salinity waters having higher bromine content than Group II. Some of these waters are associated with thick salt deposits and appear to be altered bitterns left after salt deposition. The origin of some of these waters is not known.