柴达木盆地涩北气田疏松砂岩气藏水气体积比及水侵预警

柴达木盆地涩北气田属于弱边水驱动的背斜型浅层疏松砂岩气田,采用衰竭式开采。根据水气体积比,其气藏生产过程可分为4个阶段,即低含水稳产阶段、初期水侵阶段、边水突破阶段和强水侵阶段。依照水气体积比变化,可以准确监测水侵的发生,水侵突破阶段可以作为预判边水大规模水侵的时间窗口,以调整开采方案,延长稳产期;高含水的强水侵阶段,生产周期较长,是带水开采提高采收率的重要阶段。     

高温-超压-高CO2背景下致密砂岩储层成岩作用特征——以莺歌海盆地LD10区新近系梅山组-黄流组为例

利用薄片鉴定、扫描电镜、阴极发光及碳氧同位素分析等手段,对莺歌海盆地LD10区新近系梅山组-黄流组高温-超压-高CO₂背景下的储层成岩作用特征及其对孔隙的影响进行了系统研究。研究结果表明: ①莺歌海盆地LD10区新近系梅山组-黄流组储层发育重力流沉积,岩性以中-细粒长石岩屑石英砂岩为主,储层物性以特低-低孔、特低渗特征为主。②压实、胶结和溶蚀作用是研究区主要的成岩作用类型。超压对黏土矿物的转化及石英次生加大具有明显抑制作用,并在一定程度上保护了原生孔隙。富含CO₂的高温流体不仅造成了黏土矿物的异常转化,同时促进了溶蚀作用发生,增加了次生孔隙。③研究区黄二段储层的成岩演化序列为: 菱铁矿胶结→石英次生加大→绿泥石胶结→长石淋滤溶蚀→高岭石形成→早期方解石胶结→早期白云石胶结→长石溶蚀→方解石溶蚀→伊利石大量生成→晚期铁方解石、铁白云石形成。④总体上,压实作用使孔隙度减少了45.30%～62.93%,胶结作用使孔隙度减少了1.65%～35.01%,溶蚀作用使孔隙度增加了0.72%～8.00%。其中,黄流组中下部砂岩储层受到了超压保护和CO₂溶蚀作用的双重影响,物性较好,钻井过程中应考虑高CO₂风险。     

贫铀合金的大气腐蚀特性研究

通过对贫铀合金在沿海、内地的户外暴露试验和库内露置试验，研究并得到了贫铀合金的大气腐蚀特性，分析了大气中SO2、Cl-及相对湿度腐蚀贫铀合金的原因与结果.      

引洮7~#隧洞含水疏松砂岩地层冻结法施工数值模拟

为探究含水疏松砂岩地层引水隧洞冻结施工中冻土帷幕的形成过程及力学特性,对引水隧洞的冻结施工及开挖过程进行三维数值模拟。研究了冻土帷幕的温度场、应力及位移的分布,计算出冻土帷幕完全形成所需的时间及其压、拉、剪应力极值并确定极值发生的位置。结合现场监测数据,分析了冻结过程中冻土的温度变化规律及冻土帷幕的形成机理,最后提出了相应的措施及建议。     

掏挖基础在强风化砂岩地基中的应用探讨

文章对强风化砂岩抗剪强度指标进行了分析和探讨,提出了用岩体结构面抗剪强度指标折减来获得强风化砂岩的内摩擦角和粘聚力的方法,并结合掏挖基础应用条件,通过计算掏挖基础在强风化砂岩地基应用时扩底成型稳定性,得出在强风化泥质粉砂岩和粉砂岩地区掏挖基础在施工过程中能够掏挖成型并大量应用的结论.     

RADIOIMMUNOTOXICOLOGICAL EFFECT OF ENRICHED URANIUM ON CENTRAL AND PERIPHERAL IMMUNE CELLS AND THE PROTECTIVE ACTION OF IL－1 AND IL－2

ＲＡＤＩＯＩＭＭＵＮＯＴＯＸＩＣＯＬＯＧＩＣＡＬＥＦＦＥＣＴＯＦＥＮＲＩＣＨＥＤＵＲＡＮＩＵＭＯＮＣＥＮＴＲＡＬＡＮＤＰＥＲＩＰＨＥＲＡＬＩＭＭＵＮＥＣＥＬＬＳＡＮＤＴＨＥＰＲＯＴＥＣＴＩＶＥＡＣＴＩＯＮＯＦＩＬ－１ＡＮＤＩＬ－２￥ＺｈｕＳｈｏｕｐｅ...     

A new insight into promotion action of Co2+ in Ni-diamond composite electrodeposition

A new insight into the promotion action of Co²⁺ on both particle and metal deposition in Ni-diamond composite electrodeposition system was analyzed according to electrochemical measurements. The results showed that the addition of Co²⁺ made particles content in deposits increased remarkably. The change of particles content in deposits was related inversely to the change of cathodic zero potential with the increase of the concentration of cobalt sulfate. Zero charge potential of cathode was shifted to much more negative region. The negative shift of the zero potential, combining with positive shift of the zeta potential, increased the electrostatic force between the particle-adsorbed metallic cations and the cathode. It not only benefits to the transportation of particles in solution towards cathode, but also shortens their residence time on cathodic surface. Meanwhile, entry of particles is also promoted. For metals deposition, reduction resistance of metallic cations rises greatly and deposition current at cathodic potentiodynamic polarization decreases after cobalt sulfate has been added into electrolyte. These factors are favorable for increasing particles content in deposits. In addition, physical model of diamond particles deposition state before and after the addition of Co²⁺ has been discussed.     

中条山胡—蓖型铜矿床成因新认识

讨论了剥离断层与成矿物质来源,矿体空间分布型式以及矿化特征等方面联系,从而提出胡-蓖型铜矿床是一个受剥离断层控制的“热液型(断)层状矿床”。     

Premelting transition in uranium dioxide

Thermal analysis of the cooling curves of small samples of uranium dioxide, laser heated in a high-pressure autoclave on a subsecond time scale to a temperature just below the melting point, reveals, in the case of nominally stoichiometric UO_2.00, a significant -like heat capacity peak, indicating a premelting transition in this material. The results are discussed and a simple model is presented in terms of which the observed behavior can be described.Summary of a paper presented at the Third Workshop on Subsecond Thermophysics, September 17–18, 1992, Graz, Austria. Because of its length, the full paper was published in a regular issue of this journal (Vol. 14, No. 2, 1993).     

鄂西-湘西北地区铅锌矿矿源层对铅锌矿床产出定位的制约

自鄂西至湘西北一线,自北至南铅锌矿的产出层位逐渐抬高。通过对该区矿源层的分析研究发现,矿源层层位控制了铅锌矿的产出层位,北部鄂西地区矿源层为震旦系下统陡山沱组含泥碳质碎屑岩,南部湘西地区矿源层为寒武系下统牛蹄塘组含泥碳质碎屑岩。以地层不整合界面和盆地演化的充填系列为成矿单元,下部碎屑岩地层中的铅锌矿源层制约了上部碳酸岩地层中的铅锌矿的产出定位,矿床就位是热液、矿源层、导矿构造、储矿空间、屏蔽层等多因藕合、临界转换的结果,其成因为盆源热液矿床。