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排序方式: 共有315条查询结果,搜索用时 31 毫秒
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The dispersal of metalliferous pollution from several spoil heaps produced during 20th century copper mining in the Gruben River valley, Namibia is examined. The Gruben River flows through an extremely arid environment with an average rainfall of ˜25 mm p.a. The potential for physical and chemical remobilisation of Cu, Zn and Ni is assessed by examining the spatial and temporal distribution of metal-contaminated sediment deposited within the confines of the channel. The relationships between metal content, grain size, geomorphic environment and the downstream distribution of metals are discussed. The phase-specific heavy metal concentrations of sediments, collected as part of the downstream sampling programme, are also examined using progressively more aggressive sequential acid extractions. In addition, metal concentrations are compared with Dutch guidelines for soil contamination to ascertain the extent of environmental risk.Total metal concentrations show that the Gruben valley is highly contaminated, particularly with respect to Cu and Ni concentrations, which exceed Dutch target values for Cu (36 ppm) in 94.7% and Ni (35 ppm) in 90.5% of samples, respectively. Zn concentrations are much lower with only 6.3% of the samples exceeding the target value (140 ppm). As might be expected, the metal–sediment concentrations of Cu are the most highly elevated, with a peak value of 10,500 ppm being recorded from material collected from suspended sediment transported during a minor flow event that occurred in March 1999. Lower energy and fine-grained sedimentary environments are shown to be clearly associated with higher metal concentrations. Sequential extractions of metals show that of the three principal elements considered in this study, only a negligible proportion of Cu (0.41%) is held in the exchangeable phase. Ni and Zn were below detection limits. Although the total metal concentrations in the Gruben River valley sediments are extremely high and are in themselves a concern, the small percentage of metals held in the exchangeable phase and the low potential for remobilisation under the arid conditions would suggest that they pose only a minor risk to the environment. 相似文献
64.
淄博煤矿矿坑排水的水化学特征及其形成机理的初步研究 总被引:7,自引:1,他引:6
本文讨论了淄博煤矿矿坑排水的水化学特征,指出了淄博南部和北部煤矿水化学成分的差异。通过矿坑水形成3个反应过程中水化学成分的计算,初步分析了矿坑水形成的机理:产酸作用与中和作用强度的不同是造成南、北煤矿水化学成分差别的主控机理,产酸作用的差异与煤层含硫量的高低密切相关;北部煤矿第二阶段的反应-铁氧化沉成矿 淀已进行完全或接近完全,而南部煤矿矿坑水仍富铁;参与中和作用的矿物有方解石、白云石及高岭石、绿 相似文献
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Catastrophic and dangerous inflows to salt mines in Poland as related to the origin of water determined by isotope methods 总被引:2,自引:0,他引:2
Tritium, 14C, δ13C, δ18O and δD measurements indicated as early as 1973 the existence of inflows of modern meteoric water to the Wapno salt mine
in a Zechstein diapir. In spite of these early warnings, the continuation of improper exploitation led, in 1977, to sudden
flooding of the mine followed by catastrophic land subsidence. The lesson learned from that catastrophe, as well as the results
of isotope investigations performed in the Inowrocław salt mine, led to the decision to flood the mine artificially in order
to avoid a similar land subsidence. The Kłodawa mine was not regarded to be in danger of flooding due to a thick clay cap.
In fact, a large number of usually short-lasting water occurrences had the isotopic composition characteristic for evaporated
ocean water. However, since 1956 an inflow has existed with δ18O and δD values close to that of pre-Quaternary saline waters and brines in the Mesozoic formations adjacent to the diapir.
Two other inflows have recently occurred with the initial δ18O and δD values of modern waters. As a consequence, the mine is regarded to be in danger, and the exploitation of salt in
the areas of inflows has been stopped. The Wieliczka mine, southern Poland, exploits Miocene salts overthrusted together with
the Carpathian flysch from the south. The most dangerous and catastrophic inflows were caused by human errors. Isotope data
show the water to be of glacial or Holocene age stored in Tertiary, slightly cemented rocks of low permeability, which neighbor
the mine from the north. Owing to specific geology, the mine has survived for a long time, in spite of relatively large and
long-lasting inflows. However, its existence is in permanent danger.
Received: 7 March 1997 · Accepted: 17 November 1998 相似文献
67.
从矿山生产经营的主要指标分析入手,建立以效益为目标函数的经济分析模型,全面进行矿产经济评价,探讨生产成本、出矿品位、贫化率、矿石产量等对矿山经营效果的影响,从而找出影响矿山经济效益的主要因素,进行指导矿山生产。 相似文献
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Vida Safari Gilnaz Arzpeyma Fereshteh Rashchi Navid Mostoufi 《International Journal of Mineral Processing》2009,93(1):79-83
A new mathematical model was developed for leaching of zinc ores containing silicates such as hemimorphite which produce a gel during leaching with sulfuric acid. This model is based on the shrinking core model in which the particle size and the reacting core shrink simultaneously. It was shown that the actual dissolution time of the ore particles is longer than the time corresponding to the dissolution of chemical zinc oxide itself. It was suggested that because of the existence of silicates in the ore, a gelatinous layer was formed around the reacting core. Since the gel product is soft, it breaks apart when the particles collide and as a result, the particles shrink. However, a thin gelatinous layer always covers the reacting core which increases the mass transfer resistance and increases the leaching time. This model was applied to leaching of a zinc-rich tailing containing hemimorphite and the thickness of the gelatinous layer as well as the diffusion coefficient in this layer was determined. 相似文献
70.
北京市矿山地质环境评价 总被引:1,自引:0,他引:1
通过对1443处(1661个)矿山的实地调查,采用地质环境指数法进行评估,利用ArcGIS软件,使用"natural breaks"(自然断点法)分级法,圈定出矿山地质环境影响严重区、较严重区和轻微区,提出了治理对策建议。 相似文献