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721.
Seventy-six samples of formation waters were collected from oil wells producing from the Aux Vases or Cypress Formations in the Illinois Basin. Forty core samples of the reservoir rocks were also collected from the two formations. Analyses of the samples indicated that the total dissolved solids content (TDS) of the waters ranged from 43,300 to 151,400 mg/L, far exceeding the 35,400 mg/L of TDS found in typical seawater. Cl-Br relations suggested that high salinities in the Aux Vases and Cypress formation waters resulted from the evaporation of original seawater and subsequent mixing of the evaporated seawater with concentrated halite solutions. Mixing with the halite solutions increased Na and Cl concentrations and diluted the concentration of other ions in the formation waters. The elemental concentrations were influenced further by diagenetic reactions with silicate and carbonate minerals. Diagenetic signatures revealed by fluid chemistry and rock mineralogy delineated the water-rock interactions that took place in the Aux Vases and Cypress sandstones. Dissolution of K-feldspar released K into the solution, leading to the formation of authigenic illite and mixed-layered illite/smectite. Some Mg was removed from the solution by the formation of authigenic chlorite and dolomite. Dolomitization, calcite recrystallization, and contribution from clay minerals raised Sr levels significantly in the formation waters. The trend of increasing TDS of the saline formation waters with depth can be explained with density stratification. But, it is difficult to explain the combination of the increasing TDS and increasing Ca/Na ratio with depth without invoking the controversial 'ion filtration' mechanism. 相似文献
722.
Giorgio Capasso Rocco Favara Salvatore Francofonte Salvatore Inguaggiato 《Journal of Volcanology and Geothermal Research》1999,88(3):209
Gas samples from some fumaroles at ‘La Fossa' crater and Baia di Levante on Vulcano Island and from a diffuse soil gas emission were analysed during 1995–1996, along with water samples from thermal wells in the area of Vulcano Porto. During 1996, we observed a significant increase both in the gas/steam ratio and in the CO2 concentration, as well as strong variations in δ13CCO2, δDH2O and δ18OH2O of fumarolic gases. These variations are probably related to an increased inflow of deep fluids of magmatic origin. The temperatures of fumaroles did not show remarkable variations except for fumarole F11. In this case, temperature increased by about 80°C from February to August 1996. During the same period, remarkable variations in temperature, phreatic level and chemical and isotopic composition of water were also recorded in one of the geothermal wells in the Vulcano Porto area (Camping Sicilia; T60°C). The observed variations in this well are probably related to a pressure build-up, occurring at least in the surficial part of the system, because of increased gas flux and/or decreased permeability of the fumarolic degassing system. Chemical and isotopic composition of the water showed that during this evolutionary phase, the content of fumarolic condensate in this well was about 80 to 90%. Based on the observation of physical and chemical variables of the Camping Sicilia fluids, during this phase of activity, it is concluded that this area is affected by a phreatic eruption hazard if a volcanic episode with high energy discharge in a limited time span occurs. It follows that this well may be considered as a preferential point for volcanic activity monitoring, both in the case of normal routine surveillance and in the case of inaccessibility to the crater area. 相似文献
723.
秦山核电站邻近水域浮游动物的群落结构和年际变化 总被引:2,自引:0,他引:2
描述了1995~1996年度秦山核电站邻近水域浮游动物的生物量、丰度、群落结构及其与环境因子的关系,并与1989~1990年度的资料进行了对比分析。结果表明,秦山核电Ⅰ期工程运行以来,对该水域浮游动物群落结构未产生明显的影响 相似文献
724.
伶仃河口湾铜鼓水域水沙净输运分析 总被引:7,自引:1,他引:6
根据对珠江伶仃河口湾铜鼓水域丰水期9个测站大、中、小潮三次同步水文泥沙资料及57个底质样品的分析结果,本文讨论了此水域的水沙净输运趋势。结果表明,铜鼓水域表层余流向海,浅滩测站中底层余流指向河口方向,欧拉余流主要由径流构成。沟槽悬沙输运以净平流作用为主,浅滩区则以向上游的潮抽吸输运为主。沉积物净输运趋势显示铜鼓浅滩是海陆双向底质输运的汇聚地带 相似文献
725.
东沙群岛西南海域单站潮流及温盐特征分析 总被引:1,自引:0,他引:1
利用东沙群岛西南海域定点站(20°41’N,115°49’E)3个航次观测的海流、水温资料及同期的温、盐度断面资料,用谱分析方法对该站海流、水温时间序列进行分析。结果表明,该站海流和水温的时间变化都具有明显的全日周期和半日周期波动的特征,潮流为不规则全日潮,主轴顺时针方向旋转。内潮为全日内潮占优,且具有间歇特征。和总流动类似,斜压运动也主要是顺时针方向旋转的。 相似文献
726.
727.
728.
舟山近海棘头梅童鱼群体遗传多样性微卫星DNA分析 总被引:5,自引:0,他引:5
应用6对可在棘头梅童鱼(Collichthy lucidels)中扩增的大黄鱼(Pseudosciaena Crocea)微卫星引物对浙江舟山近海的棘头梅童鱼群体进行PCR扩增,变性聚丙烯酰胺凝胶电泳分析扩增产物.6对引物在群体中共扩增出46个等位基因,平均每个位点得到5.308 0个有效等位基因,各位点的PIC值为0.412 6~0.893 5(平均值0.670 8),PC1C4和PC8F5为中度多态性位点,PC4H12、PC5E11、PC10F10及PC10G6为高度多态性位点,这些位点可以做为棘头梅童鱼群体遗传学研究的有效的分子遗传标记.6个位点的连锁分析显示,各位点间不存在明显的连锁关系.各位点在群体中的观测杂合度(Ho)为0.454 5~0.916 7(平均值0.659 1),期望杂合度(He)为0.468 0~0.901 9(平均值0.699 7),与其他海水鱼类比较,浙江近海的棘头梅童鱼群体遗传多样性偏低.对各位点进行Hardy-Weinberg平衡检测表明,PC4H12、PC10F10及PC10G6位点的等位基因频率偏离了平衡,综合现有的资源调查资料,遗传多样性的降低与近年来棘头梅童鱼资源的下降有关. 相似文献
729.
730.
南沙群岛海区晚第四纪深海碳酸盐沉积作用 总被引:5,自引:1,他引:5
根据5个柱样分析,讨论了冰期一间冰期碳酸盐沉积作用变化,南沙海区碳酸盐旋回在3500m以浅表现为大西洋旋回,源于冰期陆源碎屑物质的稀释作用,相反,在3500m以下出现太平洋碳酸钙旋回,文中根据浮游有孔虫的溶解指数和种属数量讨论了冰期-间冰期溶解作用变化。 相似文献