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141.
磷资源采矿工程对生态环境的影响及对策 总被引:2,自引:0,他引:2
处理好磷资源开采利用与生态环境保护的关系是一项关系到可持续发展的重大课题。文章以王集磷矿一、二期工程对生态环境影响为实例,研究了保护矿山生态环境的对策,进行了矿山开发事故灾害等风险分析及采矿工程环境经济损益分析,为矿区环境管理及同类型研究提供了理论和实际应用依据。 相似文献
142.
本文系统地阐述了国内外有关金矿床同位素定年方面的最新进展和古地磁法、天然裂变径迹法的基本原理 ,并对常用同位素定年法的适用性和局限性进行了评述 相似文献
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新疆乌伦古河上游地区.以出露中上泥盆统的中基性火山岩为主,这一层位是该区一个最主要的矿源层。加之存在巨大的韧性剪切带及强烈的岩浆活动而为金的富集成矿提供了可靠的地质前提;本身有希望的又有广布的金矿化点及异常点表明了它不失为一个有希望的潜在远景区。 相似文献
145.
福建省梅仙式块状硫化物矿床 总被引:1,自引:0,他引:1
梅仙式铅锌矿床是在大陆裂谷环境下形成的,有明显的块状硫化物矿床特征。矿化受震旦系龙北溪组绿片岩控制。矿体里似层状,与围岩产状一致。绿片岩原岩是一套含板内拉斑玄武岩的火山沉积建造。矿物组合和 Zn/Pb比值有分带性。层状矿体下盘有脉状、网脉状矿化和蚀变带。矿石有特征的结构构造。硫以幔源为主,铅是幔壳混合成因,矿液以海水成因为主.可能有少量雨水、岩浆水等渗入,反映物质的多来源和成矿受多种地质事件的叠加改造。本式矿床可与火山岩容矿型的加拿大新不伦瑞克省的块状硫化物矿床类比,也可作为广义华南型的一个亚型。 相似文献
146.
金属硫化物中次显微金的赋存状态已引起人们的重视。张八岭构造带蚀变构造岩型和石英脉型两类金矿金属硫化物中次显微金质子探针分析显示 ,Au与As、Fe、S、Cu、Pb呈正相关关系 ,Au以显微包裹体形式存在于金属硫化物中。与蚀变构造岩型金矿相比 ,晚期的石英脉型金矿可见自然金含量较高 ,硫化物中显微包裹体金含量较低 ,可能预示中低温热液金矿中 ,不仅普遍存在时空分异的金属硫化物中的类质同象金和自然金 ,还可能存在一定程度的时空分异的自然金和次显微包裹体金。 相似文献
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148.
大鸨生长期能量代谢和蛋白质沉积量的初步研究 总被引:8,自引:0,他引:8
对不同日龄笼养大鸨 (Otistarda)的能量代谢和蛋白质沉积量进行研究 .结果表明 ,5 0日龄、70日龄、30 0日龄和 4 0 0日龄雄性大鸨的能量日摄入量分别为 14 98.9kJ、2 376 .2kJ、2 397.4kJ和 2 4 6 5 .9kJ;能量代谢率分别为 82 .3%、81.8%、81.8%和 83.1% ;蛋白质的日沉积量分别为 5 .8g、13.4g、15 .8g和 13.5g .表 3参 9 相似文献
149.
Ronnen Levinson Paul Berdahl Asmeret Asefaw Berhe Hashem Akbari 《Atmospheric environment (Oxford, England : 1994)》2005,39(40):7807-7824
A roof with high solar reflectance and high thermal emittance (e.g., a white roof) stays cool in the sun, reducing cooling power demand in a conditioned building and increasing summertime comfort in an unconditioned building. The high initial solar reflectance of a white membrane roof (circa 0.8) can be lowered by deposition of soot, dust, and/or biomass (e.g., fungi or algae) to about 0.6; degraded solar reflectances range from 0.3 to 0.8, depending on exposure. We investigate the effects of soiling and cleaning on the solar spectral reflectances and solar absorptances of 15 initially white or light-gray polyvinyl chloride membrane samples taken from roofs across the United States. Black carbon and organic carbon were the two identifiable strongly absorbing contaminants on the membranes. Wiping was effective at removing black carbon, and less so at removing organic carbon. Rinsing and/or washing removed nearly all of the remaining soil layer, with the exception of (a) thin layers of organic carbon and (b) isolated dark spots of biomass. Bleach was required to clear these last two features. At the most soiled location on each membrane, the ratio of solar reflectance to unsoiled solar reflectance (a measure of cleanliness) ranged from 0.41 to 0.89 for the soiled samples; 0.53 to 0.95 for the wiped samples; 0.74 to 0.98 for the rinsed samples; 0.79 to 1.00 for the washed samples; and 0.94 to 1.02 for the bleached samples. However, the influences of membrane soiling and cleaning on roof heat gain are better gauged by fractional variations in solar absorptance. Solar absorptance ratios (indicating solar heat gain relative to that of an unsoiled membrane) ranged from 1.4 to 3.5 for the soiled samples; 1.1 to 3.1 for the wiped samples; 1.0 to 2.0 for the rinsed samples; 1.0 to 1.9 for the washed samples; and 0.9 to 1.3 for the bleached samples. 相似文献
150.
Schulmeister MK Healey JM Butler JJ McCall GW 《Journal of contaminant hydrology》2004,69(3-4):215-232
Discrete-depth sampling of inorganic groundwater chemistry is essential for a variety of site characterization activities. Although the mobility and rapid sampling capabilities of direct-push techniques have led to their widespread use for evaluating the distribution of organic contaminants, complementary methods for the characterization of spatial variations in geochemical conditions have not been developed. In this study, a direct-push-based approach for high-resolution inorganic chemical profiling was developed at a site where sharp chemical contrasts and iron-reducing conditions had previously been observed. Existing multilevel samplers (MLSs) that span a fining-upward alluvial sequence were used for comparison with the direct-push profiling. Chemical profiles obtained with a conventional direct-push exposed-screen sampler differed from those obtained with an adjacent MLS because of sampler reactivity and mixing with water from previous sampling levels. The sampler was modified by replacing steel sampling components with stainless-steel and heat-treated parts, and adding an adapter that prevents mixing. Profiles obtained with the modified approach were in excellent agreement with those obtained from an adjacent MLS for all constituents and parameters monitored (Cl, NO(3), Fe, Mn, DO, ORP, specific conductance and pH). Interpretations of site redox conditions based on field-measured parameters were supported by laboratory analysis of dissolved Fe. The discrete-depth capability of this approach allows inorganic chemical variations to be described at a level of detail that has rarely been possible. When combined with the mobility afforded by direct-push rigs and on-site methods of chemical analysis, the new approach is well suited for a variety of interactive site-characterization endeavors. 相似文献