海拉尔盆地贝尔凹陷兴安岭群储层粘土矿物组成及成因研究   总被引：1，自引：0，他引：1  

刘钦甫  付正  候丽华  郑丽华 《矿物学报》2008,28(1):43-47

油田注水开发是保持地层能量,提高采收率的有效手段.海拉尔地区由于粘土矿物含量高,在开发过程中储层遇水易泥化、坍塌,严重影响油气的有效开采.通过X射线衍射、偏光显微镜观察和扫描电镜分析,确定了海拉尔盆地贝16断块兴安岭群储层自上而下存在三种粘土矿物组合:蒙脱石 高岭石 (绿泥石)→高岭石 伊/蒙间层 伊利石 (绿泥石)→伊利石 绿泥石 绿/蒙间层 伊/蒙间层.粘土总量在9.1%～69.1%之间,由地层浅部到深部呈现由高到低的变化规律.详细研究了水敏性极强的钠蒙脱石及其间层矿物,认为凝灰物质的水解蚀变以及长石和中、酸性岩屑在成岩过程中的次生变化是造成海拉尔地区粘土含量高的主要因素.  相似文献   

Local Distribution and Seasonal Variation of Fe, Pb, Zn, Cu, Cd, Na, K, Ca, and Mg Concentrations in the Seagrass Cymodocea nodosa (ucria) Aschers. in the Antikyra Gulf, Greece     

P. Malea  S. Haritonidis 《Marine Ecology》1995,16(1):41-56

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麻痹性贝毒毒素研究Ⅰ.塔玛亚历山大藻的麻痹性贝毒毒素对运动神经末梢和全细胞钠离子通道的抑制作用研究     

王云峰  于仁诚  李钧  颜天  周名江 《海洋科学集刊》2003,(45):132-137

麻痹性贝毒(Paralytic Shellfish Poisoning，PSP)毒素由石房蛤毒素(saxitoxin，STX)及其衍生物组成，目前己发现20余种，在赤潮研究、分子生物学和神经生物学基础研究、医药、军事防化等方面都有应用潜力[其结构、类型和应用见本集刊王云峰等(2003)“麻痹性贝毒毒素的应用研究进展”一文]。由于PSP毒素的稀有来源和国际社会对STX交易的禁止，限制了国内PSP毒素应用及研究的全面深入展开，因此本文作者对PSP毒素进行了制备，并采用不同方法对制备的PSP毒素进行了研究。 PSP毒素能够选择性地可逆抑制可兴奋膜的电压依赖钠离子通道的开放，从而阻止神经冲动的发生和传导，使神经、肌肉丧失兴奋性(Frace et al.，1986；Penzotti et al.，1998)。本文利用神经束膜下记录和全细胞膜片钳技术，报道了从塔玛亚历山大藻(Alexandrium tamarense)中提取的PSP粗毒素对小鼠运动神经末梢膜电流和NG108-15细胞钠离子通道的作用研究结果，并与STX标准毒素的作用结果进行了比较。 NG108-15细胞是由小鼠神经母细胞瘤和大鼠胶质细胞瘤融合的杂交细胞，经分化剂分化后，显示诸+L1196如兴奋性、合成和释放乙酰胆碱、与培养肌细胞形成突触联系等多种神经细胞的基本特性(Hamprcht，1977)和Na+、K+、Ca2+等多种离子通道，已作为神经细胞模型被广泛应用于分析药物对离子通道作用的研究(Enomoto et al.，1992； Docherty et al.，1992；Shi et al.，1993；Hu et al.，1997a；Hu et al.，1997b)；发育出具有Na+内流支持的锋电位(Hamprecht,1977)，该电位是分析作用于膜钠离子通道药物的好材料。  相似文献   

褐牙鲆鳃丝Na+-K+-ATPase性质的研究   总被引：3，自引：0，他引：3  

唐贤明  潘鲁青  田景波 《中国海洋大学学报(自然科学版)》2004,34(6):969-972

研究了褐牙鲆 (Paralichthysolivaceus)鳃丝Na K ATPase的性质。结果表明 :褐牙鲆鳃丝Na K ATPase活力随着反应温度、pH的增加均呈现峰值变化 ,其最适反应温度为 3 0～ 3 5℃ ,高于 40℃酶活力急剧下降 ,至 5 0℃酶失活 ,而最适pH为 7.5～ 8.0之间 ,pH <7.5或 >8.0时酶活力急剧下降 ,低于 6.0酶活则被完全抑制 ;在本试验设计的反应时间和底物浓度范围内 ,随着时间和底物浓度的增大 ,酶活力的变化均为逐渐升高 ,且上升趋势逐渐变缓 ;反应介质中Na ,K ,Mg2 的最适浓度分别为 180 ,3 0 ,6mmol/L ,并且当K 或Mg2 浓度为 0时 ,酶活力均接近于 0。抑制剂乌本苷对鳃丝Na K ATPase活力表现为显著性抑制 ,在乌本苷浓度为 2mmol/L时 ,酶活力完全被抑制。  相似文献   

Na depletion in modern adakites via melt / rock reaction within the sub-arc mantle     

X.L. Xiong  B. Xia  J.F. Xu  H.C. Niu  W.S. Xiao 《Chemical Geology》2006,229(4):273-292

Interaction between slab-derived melt and mantle peridotite and the role of slab melt as a metasomatizing agent in the sub-arc mantle is being increasingly recognized. Adakite, the slab melt erupted on the surface, usually exhibits anomalously high MgO, CaO, Cr and Ni contents that indicate interaction with mantle peridotitite. Here we note that Cenozoic adakites have Na₂O contents below 5.8 wt.% with ∼95% samples lower than 5.0 wt.%, and are generally depleted in this component relative to experimental basalt partial melts (mostly beyond 5.0 wt.% and up to 9.0 wt.% Na₂O) produced under 1.5-3.0 GPa conditions that are most relevant to adakite production. We interpret the adakite Na depletion to be also a consequence of the melt / rock reaction that takes place within the hot mantle wedge. During ascent and reaction with mantle peridotite, primary adakite melts gain mantle components MgO, CaO, Cr and Ni but lose Na₂O, SiO₂ and perhaps K₂O to the mantle, leading to Na-rich mantle metasomatism. Selective assimilation of predominately mantle clinopyroxene, some spinel and minor olivine at high T/P has been considered to be an important process in producing high-Mg adakites from primary low-Mg slab melts [Killian, R., Stern, C. R., 2002. Constraints on the interaction between slab melts and the mantle wedge from adakitic glass in peridotite xenoliths. Eur. J. Mineral. 14, 25-36]. In such a process, Na depletion in the assimilated melt is the result of dilution due to the increase in melt mass. Phase relationships in the reaction system siliceous melt + peridotite and quantitative calculation suggest that assimilation of mantle clinopyroxene, olivine and spinel and fractional crystallization of sodic amphibole and orthopyroxene, under conditions of moderate T/P and increasing melt mass, is also an important process that modifies the composition of adakites and causes the Na depletion.  相似文献   

川滇密西西比河谷型铅锌矿床成矿流体来源研究:流体Na-Cl-Br体系的证据   总被引：11，自引：1，他引：11  

李泽琴  王奖臻  倪师军  李朝阳  胡晓强  李桃叶 《矿物岩石》2002,22(4):38-41

应用流体包裹体滤液分析方法，测定了川滇7个MVT铅锌矿床成矿流体的Na,Cl,Br含量，结果表明成矿流体的x(Na/Br)和x(Cl/Br)的平均值分别为185和73，并与高度蒸发浓缩的残留海水的x(Na/Br)和x(Cl/Br)相近。成矿流体的Na,Cl含量呈正相关，在lgNa-lgCl图解中呈线性分布。根据这些事实以及矿床地质特征，认为原始成矿卤水起源于蒸发浓缩的残留海水，原始含矿卤水与富含有机质的大气降水混合导致矿质沉淀而成矿。  相似文献   

Geochemical Characteristics of Granitoids of the Erdenet Porphyry Copper Deposit, Mongolia   总被引：4，自引：0，他引：4  

Haruhisa Morozumi 《Resource Geology》2003,53(4):311-316

Abstract. The Erdenet porphyry copper deposit is one of the major mineral deposits in Mongolia. The geochemical data of granitoids acquired for the Erdenet and its surrounding areas are re-examined. The granitoids of the Erdenet deposit with hypogene type mineralization show the lowest TiO₂ content. Although Ti was possibly lost through the pyritization, it is also possible that the hypogene type mineralization occurred accompanied with the most differentiated granitoids. The variation of the element contents related to the mineralization of the Erdenet deposit shows the decrease of MgO and CaO contents, rather constant K₂O content, rather constant to decrease of Na₂O content, with respect to the Cu contents. The rather constant Na₂O in the mineralized zone is owing to the residual albite against the sericitic alteration. The granitoids of the Erdenet area show an increase of Na₂O content and a decrease of K₂O content with an increase of SiO₂ content. This trend makes clear contrast to granitoids in the surrounding areas. The granitoids of the Erdenet area might have the adakitic nature based on the Sr and Y contents.  相似文献   

Metasomatism and the formation of greisen in Grainsgill,Cumbria, England     

D. E. Roberts 《Geological Journal》1983,18(1):43-52

A section of hornfelsed Skiddaw Slate adjacent to the margin of the Grainsgill Greisen is described and chemical analyses of the various rock types presented. The results confirm that hydrothermal fluids liberated K and Na from the granite to produce the greisen. This gave rise to K metasomatism of the adjacent hornfels and to retrogressive metamorphism over a radius of 200m from the intrusion. Na leached from the hornfels near the intrusion and that liberated during the formation of the greisen are probably the sources of the Na in the brines recorded in fluid inclusions within the nearby quartz-tungsten veins.  相似文献   

Effects of salinity fluctuation amplitudes on growth, osmolarity, Na＋-K＋-ATPase activity and Hsp70 of juvenile Chinese shrimp Fenneropenaeus chinensis Osbeck     

丁森  王芳  董双林  高勤峰 《中国海洋湖沼学报》2009,27(4):723-728

The effects of various salinity fluctuation amplitudes (2, 4, 6 and 8) on the growth, osmolarity, Na⁺-K⁺-ATPase activity and Hsp70 of juvenile Fenneropenaeus chinensis cultured in seawater with a salinity of 20 were studied. The results show that weight gain in the salinity fluctuation treatments was better than that in control; in particular, the weight gain of treatments S4 and S0, at 231.8% and 196.3%, respectively, was significantly different (P<0.05). The hemolymph osmolarity of treatments S0, S2, S4, S6 and S8 was 635.4, 630.8, 623.6, 614.4 and 600.3 mOsm/kg, respectively, and decreased with increasing salinity fluctuation amplitude. The level of Na⁺-K⁺-ATPase activity in gills of F. chinensis was higher than that in hepatopancreas, but there were no significant differences among all treatments, either in gills or hepatopancreas (P>0.05). The relative level of Hsp70 in treatment S4 was 48.4% and 40.4% higher than control in muscle and eyestalks, respectively, with the highest values being recorded under a salinity fluctuation amplitude of 4.  相似文献   

悬浮物对半滑舌鳎(Cynoglossus semilaevis)幼鱼肝脏溶菌酶、超氧化物歧化酶和鳃丝Na⁺-K⁺-ATPase活力的影响     

周勇  马绍赛  曲克明  傅雪军  徐勇 《海洋与湖沼》2009,40(3):367-372

在实验室条件下构建不同的悬浮物浓度环境,采用试剂盒分析方法研究了不同浓度悬浮物对半滑舌鳎幼鱼肝脏溶菌酶（LSZ）、超氧化物歧化酶（SOD）和鳃丝Na^＋-K^＋-ATPase活力的影响。养殖水体中悬浮物浓度添加量分别为0（对照）、50、100、200和400mg／L,每5天采样测定一次,实验周期为25天。结果表明,当悬浮物浓度添加量为50和100mg／L时,肝脏LSZ和SOD活力与对照组无显著差异（P〉0．05）,当添加量为200和400mg／L时,肝脏LSZ和SOD活力与对照组有显著差异（P〈0．05）;实验后期各实验组鳃丝Na^＋-K^＋-ATPase活力与对照组均有显著差异（P〈0．05）。在悬浮物效应的25天内,各实验组肝脏LSZ活力呈峰值变化,10天时除100mg／L浓度添加组外均达到最大值;而肝脏SOD活力在50和100mg／L浓度添加组略有升高,在200和400mg／L浓度添加组则基本呈下降趋势;鳃丝Na^＋-K^＋-ATPase活力前10天各实验组较对照组无显著变化,之后则显著降低,后期基本趋于稳定,其活力低于初始水平;实验结束时,各实验组其肝脏LSZ、SOD和鳃丝Na^＋-K^＋-ATPase活力相对于对照组都受到了不同程度的抑制,其中各实验组鳃丝Na^＋-K^＋-ATPase活力抑制率分别达到了27．6％、65．2％、57．0％和71．1％。  相似文献