黄浦江口氯化物预报公式的初步探讨

黄浦江是上海人民生活和生产的主要水源,咸水入侵会影响黄浦江水质,给上海带来很大的危害。本文在分析黄浦江咸水入侵规律的基础上,利用吴淞水厂1973～1979年的实测资料,选取枯季月瞬时最大氯化物值为因变量,运用多元逐步回归及相合非参数回归方法,建立了黄浦江口的氯化物预报公式,取得了比较满意的结果。     

Interaction of fluid dynamic factors in the migration and accumulation of natural gas

The migration of fluid petroleum gas, described as fluid potential, depends only on gravity, fluid pressure controlled by depression and capillary force during tectonically stable period; but on tectonic stress during the tectonically active period with severe compression. This method is applied in the Junggar Basin, showing that the migration of Jurassic gas during Cretaceous and Eocene and the migration of Permian gas from Jurassic till the present are determined by capillary force and fluid pressure (including overpressure) which is controlled by depression; the migration of Jurassic gas from Eocene till the present and the migration of Permian gas during Triassic are controlled by tectonic stress.     

Composition of sandstone and heavy minerals implies the provenance of Kuqa Depression in Jurassic, Tarim basin, China

The petrological characteristics and heavy mineral assembly of the Jurassic System in Kuqa Basin are consistent with the tectonic evolution, which is the major factor controlling the filling process of Kuqa Basin. Controlled by the source areas at the both sides of the Basin, the matrixes are dominated by sedimentary rock, high-grade metamorphic rock, acid magmatic rock, and the highest heavy mineral assemblage of zircon-garnet-magnetite in the content. According to heavy mineral indexes, the Jurassic strata can be classified into three rhythmic units of heavy mineral. The lower sequence contains abundant heavy minerals and relatively high content of detritus and its matrixes primarily came form the recycling orogen. The assemblage of “zircon-garnet-magnetite” indicates that the sedimentary area in the early evolution period of the basin is relatively near the provenance. The middle sequence is different from the lower sequence in the heavy mineral assemblage and has the different characteristics from that of source rock. The heavy mineral assemblage is “garnet-zircon” with the highest content of garnet and its main matrices are the high-grade metamorphic rock, acid magmatic rock and hydrothermal vein at the northeastern edge of the basin. The middle and upper sequences are characterized by the clast provenance, which is primarily from the recycling orogen at the northern edge of the basin and secondarily from the southern uplift. As a result of the two provenances, the strata with apparent changes of heavy mineral assemblage and index better coincides with the interfaces of the secondary strata sequences, which reflects the denudation history and the filling process of the orogen at the northern edge of the basin.     

A mathematical model for solid liquid and mass transfer coupling and numerical simulation for hydraulic fracture in rock salt

Thehydraulicfracturingtechniqueiswidelyused intheoilengineering,naturalgasexploiting,under groundheatextractingandothermineralresources mining,etc.withwelldevelopedhydraulicfracture modelsforordinaryrocks[1—3].Inthefieldofsolu tionminingofsaltdeposit,thistechniqueisusedto producefracturealongtheplanelayerofthedeposit,thustoconnecttheinjectionandtargetwells[4,5].However,duetothespecialphysicalandmechanical characteristicsofrocksalt,executinghydraulicfrac tureinrocksaltdepositisdifferentfromtha…     

盐胁迫对三角滨藜种子萌发和幼苗生长的影响

通过NaCl溶液培养和海水浇灌处理，研究了盐胁迫对三角滨藜种子萌发和幼苗生长的影响．结果表明，随NaCl溶液浓度的提高，三角滨藜种子萌发有下降趋势，但低于140mmol／L NaCl溶液对三角滨藜种子萌发无明显影响；高浓度盐胁迫对三角滨藜的幼苗生长表现出抑制作用；低浓度盐胁迫（低于100mmol／L NaCl溶液培养或25％海水浇灌）则能促进其营养生长．     

Helium isotopic compositions in fluid inclusions of the Gangxi fault belt in the Huanghua Depression, Bohai Bay Basin

Helium is a trace constituent in natural gases and is the lightest element of all rare gases. Formed during natural nuclear processes, helium is chemically stable. Due to its strong diffusibility and permeability, helium can be used as a very sensitive tracer. Helium has two natural stable isotopes, 3He and 4He. 3He originates from the universal nebulae when the earth was formed, and 4He mainly originates from the radioactive disintegration of elements in the crust, such as U and Th [1]. In…     

难溶性盐钙芒硝在碱液中溶解特性的实验研究

在分析钙芒硝矿的化学组成和其溶解原理的基础上,通过实验研究了钙芒硝矿在不同碱性溶液中和不同溶解条件下溶解特性。结果表明,钙芒硝在碱性溶液中的溶解速度比较快,由于部分Na2SO4是由化学反应产生,因此属于化学溶解的范畴;钙芒硝在碱性溶液中的溶解速度与碱性强弱有关,碱性强溶解速度快,反之较慢;在溶解过程中会产生微溶物CaSO4,决定了钙芒硝在溶液流动的情况下速度较静态溶液的溶解速度快;实验结论的得出为较难溶于水的钙芒硝矿的地下水溶开采提供了一种有益的方法。     

真红树和半红树植物体内盐分分布的比较研究

研究了典型的真红树植物(红树Rhizophora apiculata、木榄Bruguiera gymnorhiza、海桑Sonneratia caeseolaris、桐花树Aegiceras corniculatum、白骨壤Avicennia marina)、半红树植物(黄槿Hibiscus tiliaceus、水黄皮Pongamia pinnata)和目前还存在争议的物种银叶树(Heritiera littoralis)体内各器官的K、Na、Cl元素分布特征.结果表明:(1)真红树植物和半红树植物体内盐分分布存在明显的区别,真红树植物体内各器官的Na、Cl含量明显比半红树高,叶片的K/Na值比半红树低;(2)真红树植物(除红树和木榄)和半红树植物的K:Na离子吸收选择性(USR)没有差异,但半红树植物的K:Na离子运输选择性(TSR)明显比真红树高;(3)真红树植物根系Cl含量随径级增加有先上升后下降趋势,与半红树植物不同.从盐分分布特征来看,银叶树最好归为半红树植物.     

香山群沉积岩浆记录及其反映的大地构造环境

目的探讨鄂尔多斯西南边缘香山群形成的大地构造环境,为鄂尔多斯盆地西南缘早古生代大地构造背景的恢复和确定提供佐证。方法通过香山群地层的岩石学、沉积学、砂岩和火山岩的岩石地球化学特征的系统研究,综合分析香山群形成的大地构造环境。结果香山群的时代划归为中晚寒武世较合适;香山群主体是一套由板岩、细、粉砂岩和砂岩组成的浊积岩系,其砂岩类型主要是长石石英砂岩、细粒石英砂岩和粉砂质石英砂岩,前寒武纪变沉积岩和花岗片麻岩为主要碎屑来源和物源区组成;砂岩的岩石地球化学特征指示香山群属发育在被动大陆边缘斜坡环境中的沉积物,火山岩岩石地球化学特征反映其应属大洋扩张构造环境下的大洋拉斑玄武岩系列。结论香山群形成于伸展构造背景下的被动大陆边缘中的大陆斜坡和深海平原环境。