河北丰宁隐爆角砾岩型银多金属矿床地质特征

河北丰宁银多金属矿床赋存于隐爆角砾岩体中,发育一组典型低温热液矿物组合的围岩蚀变,矿化为典型低温热液成因的黄铁矿-闪锌矿-方铅矿-黄铜矿硫化物组合;控矿隐爆角砾岩划分为震裂花岗岩相、震碎花岗岩相、熔浆角砾岩相和气爆角砾岩相4类;宏观、微观研究认为其中的硅质角砾由4次喷发作用形成;气爆形成的萤石化可确定赋矿空间的分布规律.     

The behavior of iron,manganese and silicon in the Peconic River estuary,New York

The behavior of dissolved and particulate iron and manganese and dissolved silicon has been studied as a function of chlorinity in the Peconic River estuary, New York. This study sought to identify important geochemical processes in a relatively pristine estuary facing increasing anthropogenic impact.Dissolved iron behaved in the classical non-conservative manner exhibiting removal of nearly 80% at very low chlorinities, while particulate iron increased by a corresponding amount over the same chlorinity range. Dissolved manganese was enriched by up to 200% over its predicted concentration at low and intermediate chlorinities by desorption from suspended particulates and by a probable benthic flux. Dissolved silicon was enriched by up to 100% at low and intermediate chlorinities also from a probable benthic flux. These fluxes were estimated to be 5 μg cm^?2 day^?1 for dissolved manganese and 70 μg cm^?2 day^?1 for dissolved silicon.The quantity of both particulate iron and manganese increased at high chlorinities due to an influx of suspended inorganic particulates. In the intermediate to high chlorinity region, oxidation of sediment-derived manganese is believed to contribute to the observed increase in particulate manganese.Total iron was essentially conservative throughout most of the estuary, while total manganese was non-conservative presumably due to extensive remobilization of dissolved manganese from the sediments.     

Mosaic and gradient SiGe single crystals for gamma ray Laue lenses

Both Ge_1−x Si _x mosaic crystals and Si_1−x Ge _x crystals with gradient of composition could be grown using the modified Czochralski technique to produce the diffracting elements for the MAX gamma ray telescope. Although many elements cut from the mosaic crystal and used before for CLAIRE gamma ray telescope had an efficiency up to 20%, the overall efficiency of the lens was about 8.1 ± 0.7 %, which is more than twice lower than the theoretically predicted efficiency. Some causes of this behaviour are discussed. In addition to mosaic crystals, the growth of Si_1−x Ge _x crystals with a gradient of composition and their properties are analysed. Such composition-gradient crystals could be a promising way to improve the diffraction efficiency of Laue lens for MAX.     

硅肥在黄河冲积土上的水稻肥效试验研究

试验研究结果表明：无论以炼铁水淬渣还是以赤泥为基料生产的硅肥,在河南省黄河冲积平原水稻上施用均获得１５％以上的增产效果,尤以赤泥的基本原料生产的硅肥增产效果最佳。     

草莓施用硅肥效果研究

对硅肥在草莓上施用效果进行了对比试验研究。结果表明,硅肥对草莓的生长发育和产量的提高有较大的作用,硅肥能够促进草莓的营养生长,使草莓株高增加１．９￣２．５ｃｍ,硅肥能促进草莓的果实增大,使外观鲜红圆润、有光泽,经济价值提高。施用硅肥可使草莓产量增加１９．１％￣２８．７％。     

盐渍土冬小麦施用硅肥效应的试验研究

通过对盐渍土施用硅肥后土壤及作物中氮、磷、钾、硅等营养元素的分析，发现施硅肥后土壤中的碱解氮、速效磷、速效钾和有效硅含量都有明显提高，小麦茎杆和籽粒中的氮、磷、钾、硅的含量也比对照处理的含量高，小麦抗逆性、光合作用等都有明显改进，增产幅度达22．7％；最后简要说明了硅肥对盐渍土的改良作用。     

The teleconnection between marine silicon supply and desertification in China

Desertification has been notably expanding in China in the recent decade, especially in North China where dust/sand storm (DSS) frequently assaulted local communities. Analyses in marine ecology found that the earth ecosystem could be able to complement nutrient silicon for keeping sustain- able development of marine ecosystem, and decreasing CO2 concentration in the atmosphere; as a result, the area of desertification would be enlarged. Modern human being activities have resulted in constant changes in the amount of silicon transport from land into sea, leading to oversupply of nitrogen and phosphorus but silicon in seawater. The proportion of nitrogen, phosphorus and silicon was seriously im- balanced and the limitation of silicon for phytoplankton growth has become more serious. The silicon de- ficiency has damaged the marine ecosystem in coastal regions and slowed down the carbon sedimentation in the atmosphere of the world. The authors believe that the continual discharge of CO2 into the atmos- phere is the cause for the global warming including marine water temperature rise. Consequently, the earth ecosystem would have to trigger its complementary action to resume to the silicon balance by algae bloom in seawater for reducing air and water temperatures. In order to complement nutrient silicon into the sea, the ecosystem would transport silicon via the atmosphere; therefore, the desertification in the in- ner land is a natural reaction. As marine phytoplankton booming can reduce the CO2 concentration in the atmosphere and further ease the green-house effect, during this process, a large amount of silicon are de- manded by the ecosystem, which human being are unable to stop desertification from happening but slow down the progress and ease the risk. Therefore, as an important role in earth ecosystem, people should reduce the CO2 discharge into the atmosphere first; then, the normal function of river transporting silicon must be restored. In this way, the CO2 in the atmosphere can be kept in balance, the global warming slowed down, marine ecosystem development sustained, the drought in inner land eased, and the desert gradually under-controlled.     

利用高精度重磁法对“羊里磁异常”的解释探讨

"羊里磁异常"自1967年发现以来,由于所处地质环境为矽卡岩型铁矿成矿有利地段,且紧邻已知的温石埠铁矿,以及"羊里磁异常"规模较大且具备低缓磁异常的特点,一直受到地质界的广泛关注,地勘单位在该区做了大量的铁矿找矿工作,但对"羊里磁异常"勘查中一直未取得突破性进展,该文从高精度重磁角度对"羊里磁异常"进行了定量解释以及定量计算,并通过钻探验证等技术手段,进一步推断"羊里磁异常"是由古近纪含磁铁碎屑的砂砾岩以及闪长岩共同引起的,对该异常的认识更进了一步。     

EXAMINATION OF SILICATE LIMITATION OF PRIMARY PRODUCTION IN JIAOZHOU BAY, CHINA I. SILICATE BEING A LIMITING FACTOR OF PHYTOPLANKTON PRIMARY PRODUCTION

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华北蓟县中元古界剖面中燧石条带的形成机制——硼硅同位素证据

天津蓟县中新元古界海相沉积碳酸盐岩建造中分布大量燧石条带,特别是雾迷山组燧石条带与白云岩互层密集产出,沉积韵律非常明显,记录了其形成时海洋的化学和生物等信息,但关于其成因和形成机制还存在不同的认识。我们对蓟县中元古界剖面中碳酸盐岩的硼同位素和燧石条带的硅氧同位素进行了系统研究。燧石条带的 δ 30 Si NBS 28 值为0. 6‰~3. 3‰,平均2. 2‰,较热水化学沉积硅质岩的 δ 30 Si NBS 28 值显著偏高,与浅海生物沉积硅质岩的硅同位素组成相近。燧石条带的 δ 18 O V SMOW 值为21. 7‰~27. 8‰,平均25. 5‰,较热液成因硅质岩的值明显偏高,而与常温海相硅质岩的 δ 18 O值相似。蓟县剖面白云岩和灰岩等碳酸盐岩的 δ 11 B SRM 951 值为0‰~11. 0‰之间,平均4. 8‰,较现代海相碳酸盐的值明显偏低。高于庄组至雾迷山组燧石条带白云岩的 δ 11 B值普遍高于白云岩和灰岩的值,在3. 3‰~12. 9‰之间,平均8. 4‰。在酸性条件下富集重硼同位素的B(OH) 3掺入碳酸盐的比例增加,可导致其 δ 11 B值升高。这表明燧石条带白云岩可能形成于局部酸性水环境。结合碳酸盐和SiO 2溶解/沉淀与pH之间相互关系,提出蓟县剖面中的燧石条带是一种具有时代特征的同沉积的生物化学沉积硅质岩。中元古代海水中SiO 2浓度高,基本呈饱和状态,Mg/Ca比值高,生物活动已成为影响海洋环境的重要因素。在生物活动繁盛期大量有机质沉积于海底,导致海水-沉积物界面附近pH值大幅下降(pH＜7. 8),白云石等碳酸盐溶解度升高,难以沉淀;与此相反,SiO 2溶解度降低,达到过饱和,大量沉淀形成燧石条带/透镜体。生物活动羸弱期,海底pH值升高恢复到正常水平,SiO 2溶解度升高,碳酸盐溶解度降低,形成白云岩等碳酸盐沉淀。生物活动的周期性变化,则形成白云岩与燧石互层的条带状韵律层。燧石条带白云岩的硼同位素组成反映的是局部流体的 δ 11 B和pH值,不适合用来反演海水的硼同位素组成。