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专辑
网络首发:2000-12-25,
纸质出版:2000
移动端阅览
塔里木盆地北部西达里亚、塔河1号及塔河3
4号油田的油田水具有相近的离子组成
其可溶物质主要成分与海水一致
表明其主要为海相成因。油田水中不同的离子组成及浓度指示特定的地质意义:HCO
3
-
与地层密度具有良好的正相关关系
地层时代愈老
直线斜率愈大;SO
4
2-
Ca
2+
Mg
浓度的差异预示油田水的不同来源;I
含量不受地层岩性影响
而由原油物性决定
I
含量高
则原油物性就好;Br
浓度大于350mg/L的油田水则是凝析油的特征。
The oilfield water in xidaliyia
Tahe-1
Tahe-3 and Tahe-4 Oilfields in Northern Tarim Basin has similar ionic composition
and the principal compositions of soluble materials are consistent with sea water
suggesting its marine origin.The different ionic compositions and concentration indicate different geological features.HCO
has positive coherence with the strata density
the concentration differences of SO
indicate different origin of the water.The content of I
is determined by physical features of crude oil but not lithologic feature
and bears negative coherence with the density of crude oil.When concentration of Br
in oilfield water is more than 350 mg/L
the oil would be condensate oil.
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