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111.
Daniel Markewitz Ricardo de O. Figueiredo Eric A. Davidson 《Journal of Geochemical Exploration》2006,88(1-3):214
The objective of this study was to investigate the role of dissolved CO2 (H2CO3*) as a mechanism of cation removal from surface soils under secondary land uses in the tropics. Soil leachate columns were prepared with 0–10 cm soils from mature and secondary forest, and managed pastures, and extracted with H2CO3* from deionized water equilibrated with 0%, 0.5%, 1%, and 10% CO2 (g). Extraction of soil cations slowed over time following an exponential form for the cumulative data. The rate of cation concentration decline varied as a function of CO2 concentration with the 10% solution resulting in a greater percent decline with extraction volume. Potassium removal from the exchange sites of all soils and for all solutions was nearly complete ranging from 85% to 97% while removals of Mg (31% to 71%) and Ca (12% to 42%) were lower. The asymptotic patterns of cation loss observed in this study suggest that H2CO3* acid-driven losses of cations may become self-limiting over time. Other stronger acids from atmospheric deposition or organic sources may serve to perpetuate cation removal, and re-forestation on these cleared lands would certainly re-distribute cations from soils to vegetation. 相似文献
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The role of saline solution properties on porous limestone salt weathering by magnesium and sodium sulfates 总被引:4,自引:0,他引:4
Saline solution properties, viscosity in particular, are shown to be critical in salt weathering associated with sodium and
magnesium sulfate crystallization in porous limestone. The crystallization of sodium and magnesium sulfate within a porous
limestone has been studied at a macro- and microscale using different techniques, including mercury intrusion porosimetry,
environmental scanning microscopy and X-ray computed tomography. Such analysis enabled the visualization of the crystallization
process in situ, and at high magnification, yielding critical information as to where and how salts crystallize. Sodium sulfate
decahydrate (mirabilite) tends to crystallize in large pores as euhedral micron-sized crystals formed at low supersaturation
near to the surface of the stone. In contrast, magnesium sulfate heptahydrate (epsomite) tends to precipitate as anhedral
wax-like aggregates formed at high supersaturation and distributed homogeneously throughout the stone pore system filling
large and small pores. While the former crystallization behavior resulted in scale formation, the latter led to crack development
throughout the bulk stone. Ultimately, the contrasting weathering behavior of the two sulfates is explained by considering
differences in flow dynamics of solutions within porous materials that are mainly connected with the higher viscosity of magnesium
sulfate saturated solution (7.27 cP) when compared with sodium sulfate saturated solution (1.83 cP). On the basis of such
results, new ways to tackle salt weathering, particularly in the field of cultural heritage conservation, are discussed. 相似文献
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研究了普通氢氧化镁(MH)、六角片状MH和硬脂酸改性MH分别填充聚丙烯(PP)复合材料的性能。用FTIR、SEM和TG对上述3种类型MH及其复合材料的结构和形貌进行了分析。试验结果表明:相比普通MH,六角片状MH和硬脂酸改性后的MH有效降低了表面极性,大大降低了对复合材料的力学性能的影响,显著提高了复合材料的热稳定性;4%SA改性MH比6%SA改性MH填充PP,界面相容性好,对复合材料力学性能的影响小。硬脂酸湿法表面处理氢氧化镁改性的最佳条件为:硬脂酸用量4%,处理温度85~90℃,处理时间60 min,料浆浓度10%。 相似文献
118.
辽东后仙峪地区元古界超镁橄榄岩岩石学及其成因 总被引:2,自引:0,他引:2
超镁橄榄岩是作者在辽东大石桥后仙峪地区发现并命名的一种新类型岩石,是以镁橄榄石分子组成为标准而定义、阳离子过剩的一种岩石。由于阳离子过剩而形成独立的铁镁氧化物矿物,因此岩石的主要矿物为镁橄榄石、硅镁石、水镁石及磁铁矿。该超镁橄榄岩中矿物呈粒状、板状结构,具有角砾状火山喷发构造、类鬣刺状熔岩冷凝构造及团块状熔离构造。岩石具有分层现象,下部为镁橄榄岩,上部为磁铁矿硅镁石岩,其中含有镍黄铁矿,并构成海绵陨铁结构。岩石学研究表明这是一套富镁质超基性火山岩,相当于科马提岩,作为辽东硼矿的容矿岩石,它为镁硼酸盐矿床的形成提供了丰富的镁质来源。 相似文献
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无机材料在国民经济和国防建设中均占有重要地位。简单介绍了一种重要的新型无机功能材料——硼酸铝晶须的性能、制备和应用前景。 相似文献