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791.
汞和镉在土壤中的吸附和运移研究进展 总被引:20,自引:2,他引:20
介绍了国内外近年来对重要的污染元素汞和镉在土壤中吸附和运移方面的研究成果。评价土壤吸附重金属离子多运用Langmuir、Freundlich及Temkin三种等温吸附曲线。影响土壤吸附汞和镉的因素主要有pH值、有机质、氯离子、土壤组分、土壤类型、竞争吸附离子的参与等。汞的活动性较差,其迁移性质缺乏研究;土壤中镉的二价离子在粘土衬层内的迁移过程中,可生成难溶性沉淀物质,阻碍了液体的渗透,因而导致渗透系数比纯水还低。引用参考文献45篇。 相似文献
792.
793.
研究了P350在硫酸介质中吸附铼的性能和微色谱柱分离微量铼的条件和选择性,确定了以P350萃淋树脂为固定相,硫酸溶液为流动相萃取色谱分离微量铼的最佳条件,以2mol/L硫酸为上拄液,4mol/L硫酸为淋洗液,水为解析液,使铼与铀(Ⅵ)、钼(Ⅵ)、铁(Ⅲ)、锰(Ⅱ)、铬(Ⅵ)、钛(Ⅳ)等金属离子分离。采用丁基罗丹明B光度法测定铀矿石中微量铼,分析结果符合要求。 相似文献
794.
795.
Jia Jianye 《中国地质大学学报(英文版)》1998,9(3):2
Surfacemineralogyisoneofthemodernbranchesofmin-eralogy.Theresearchoftheinterfaceofmineral-liquid,namelythestudyonthereactiono... 相似文献
796.
蒙脱石对黄曲霉毒素B1的吸附作用 总被引:5,自引:0,他引:5
试验研究了蒙脱石对黄曲霉毒素B1的等温吸附,以及赖氨酸、酸碱度、温度、离体肠管吸收和透析袋透析对其吸附的影响。结果表明:蒙脱石在pH2.0和pH8.0时对黄曲霉毒索B1的最大吸附量分别为613.5和628.9μg/g;赖氨酸含量为2~4mg/mL时对吸附无影响;酸碱度在pH2.0至pH8.0及温度在20℃至60℃时对吸附无明显影响;蒙脱石可减少离体肠管对黄曲霉毒素B1的吸收率及黄曲霉毒素B1通过透析袋的透析率。鸡小肠对黄曲霉毒素B1存在主动吸收过程。在吸附反应的初始阶段,蒙脱石对黄曲霉毒素B1的吸附符合一级吸附动力学方程,黄曲霉毒素B1半衰期为6.3~7.3min;20min后达到吸附平衡。 相似文献
797.
Mechanistic roles of soil humus and soil minerals and their contributions to soil sorption of nonionic organic compounds from aqueous and organic solutions are illustrated. Parathion and lindane are used as model solutes on two soils that differ greatly in their humic and mineral contents. In aqueous systems, observed sorptive characteristics suggest that solute partitioning into the soil-humic phase is the primary mechanism of soil uptake. By contrast, data obtained from organic solutions on dehydrated soil partitioning into humic phase and adsorption by soil minerals is influenced by the soil-moisture content and by the solvent medium from which the solute is sorbed. 相似文献
798.
Akiko UCHIDA Takushi YOKOYAMA Yoshinobu MOTOMURA Akane MIYAZAKI Yoshihiro OKAUE Koichiro WATANABE Eiji IZAWA 《Resource Geology》2002,52(3):223-230
Abstract: The adsorption of gold on iron(III) and aluminum hydroxides from solutions containing Au(III) complexes has been studied as a function of pH and chloride concentration at 30C. Iron(III) hydroxide was more effective in adsorbing gold from solution than aluminum hydroxide. However, both hydroxides controlled the behavior of Au(III) complex with very similar manner. The most effective gold adsorption occurred in aqueous solution with near neutral pH and low Cl concentration. In this solution condition, Au(III) complexes were mainly dissolved as AuCl2 (OH)2 - and AuCl(OH)3 - , and the surface charge for both hydroxides was positive. In addition, the adsorbed Au(III) complexes were spontaneously reduced to elemental gold in spite of the absence of a specific reducing agent.
The results of this study suggest that adsorption and spontaneous reduction of gold complexes on the surface of hydrous metal oxides with positive charge play an important role in gold precipitation in subsurface environment. 相似文献
The results of this study suggest that adsorption and spontaneous reduction of gold complexes on the surface of hydrous metal oxides with positive charge play an important role in gold precipitation in subsurface environment. 相似文献
799.
800.
REE Mineralization of Weathered Crust and Clay Sediment on Granitic Rocks in the Sanyo Belt,SW Japan and the Southern Jiangxi Province,China 总被引:1,自引:0,他引:1
Rare earth element (REE) geochemistry and mineralogy have been studied in the weathered crusts derived from the Early Yanshanian (Jurassic) biotite granites of Dabu and Dingnan, as well as in the Indosinian (Permian) muscovite–biotite granite of Aigao in southern Jiangxi province, China, and the weathered crusts and clay sediments on biotite granites in the Sanyo belt, SW Japan, that is, Okayama, Tanakami, and Naegi areas. In all of the weathered crusts, biotite and plagioclase commonly tend to decrease toward the upper part of the profile, whereas kaolinite and residual quartz and K‐feldspar increase. The weathered crusts of the Dingnan granites and some Naegi granites, which are characterized by the enrichment in light REE (LREE) in C horizons, have higher total REE (ΣREE) content than the parent REE‐enriched granites. Weathering of LREE‐bearing apatite and fluorocarbonates in the Dingnan granites and allanite and apatite in some Naegi granites may account for the leaching of LREE at the B horizons. The leached LREE must result in subsequent enrichment of LREE in the C horizons. The enrichment is probably associated with mainly adsorption onto kaolinite and partly formation of possible secondary LREE‐bearing minerals. In Japan it was found that REE mineralization occurs not in the weathered granitic crusts but in reworked clay sediments, especially kaolinite‐rich layers, derived mainly from the weathering materials of REE‐enriched granitic rocks. The clay sediments are more enriched in LREE, which likely adsorbed onto kaolinite. Concentration of heavy REE within almost all the weathered crusts and clay sediments, however, may reflect mainly residual REE‐bearing minerals such as zircon, which originated in the parent granitic rocks. The findings of the present study support the three processes for fractionation of the REE during weathering: (i) selective leaching of rocks containing both stable and unstable REE‐bearing minerals; (ii) adsorption onto clay minerals; and (iii) presence of possible secondary LREE‐bearing minerals. 相似文献