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61.
南海北部海区水团的判别分析 总被引:1,自引:0,他引:1
将判别分析应用于南海北部海区的水团分析。划分为八个水团:沿岸冲淡水团(F),近岸混合水团(M),暖表层水团(WS),表层水团(S),表—次层混合水团(SU),次层水团(U),次—中层混合水团(UI)和中层水团(I)。给出了各水团在四季代表月的Bayes多组判别的系数和参数。用资料检验判别的成效.冬季和春季可达95.90%以上,夏季为94.80%,秋季是全年最低值,为92.72%。讨论了造成错判的原因,并与Fisher判别作了比较。当测值维数较低时,建议选用Bayes判别。对八个水团以及各水团两两之间差异的显著性进行了检验,证实在每个季节中各水团之间的差异,都在高度置信水平(α=0.01)上具有显著性。因而,划分为八个水团是有实际意义的,其判别式的系数和参数,可用于实际的判别和预报。 相似文献
62.
B.L. Herzog R.A. Griffin C.J. Stohr L.R. Follmer W.J. Morse W.J. Su 《Ground Water Monitoring & Remediation》1989,9(2):82-89
Ground water contamination was discovered in 1981 in a monitoring well at the Earthline disposal facility near Wilsonville, Illinois. Organic chemicals had migrated at a rate 100 to 1000 times greater than predicted when the site received its permit to operate in 1978. Postulated failure mechanisms included migration through previously unmapped permeable zones, subsidence of an underground mine, organic-chemical and clay-mineral interactions, acid-mine drainage and clay interactions, trench-cover settlement, and erosion.
In this investigation, the Illinois State Geological Survey found the primary reason for the rapid migration: the presence of previously undetermined fractures and joints in glacial till. The inaccurate predictions of hydraulic conductivity were based on laboratory-determined values that did not adequately measure the effects of fractures and joints on the transit time calculations. Field-measured hydraulic conductivity values were generally 10 to 1000 times greater than their laboratory-measured counterparts, thus largely accounting for the discrepancy between predicted and actual migration rates in the transit time calculations. The problem was compounded, however, by the burial of liquid wastes and by trench covers that allowed excess surface runoff to enter the trenches. Organic-chemical and clay-mineral interactions may also have exacerbated the problem in areas where liquid organic wastes were buried. 相似文献
In this investigation, the Illinois State Geological Survey found the primary reason for the rapid migration: the presence of previously undetermined fractures and joints in glacial till. The inaccurate predictions of hydraulic conductivity were based on laboratory-determined values that did not adequately measure the effects of fractures and joints on the transit time calculations. Field-measured hydraulic conductivity values were generally 10 to 1000 times greater than their laboratory-measured counterparts, thus largely accounting for the discrepancy between predicted and actual migration rates in the transit time calculations. The problem was compounded, however, by the burial of liquid wastes and by trench covers that allowed excess surface runoff to enter the trenches. Organic-chemical and clay-mineral interactions may also have exacerbated the problem in areas where liquid organic wastes were buried. 相似文献
63.
厦门海区潮间带海洋动植物共附生微生物的抗菌活性 总被引:20,自引:0,他引:20
从厦门海区潮间带石纯、浒苔、江蓠、海兔、海葵及鲨鱼肠道分离得289株共附生微生物,以8种敏感菌为指示菌,从中获得拮抗活性的幼苗28株,放线菌17株,真菌8株。拮抗细菌以假单胞菌(39%)、弧菌(25%)和芽直菌(14%)为主,主要为抗革兰氏阳性细菌,抗真菌的菌株比例较低。拮抗放线菌分属于链霉菌和小单孢菌,其抗革兰氏阳性菌、阴性菌和真菌的菌株比例分别为65%、47%和23%。拮抗真菌分青霉属和芽枝霉 相似文献
64.
全新世岱海流域化学风化及其对气候事件的响应 总被引:12,自引:0,他引:12
通过对岱海 12.08 m沉积岩芯 210Pb和 AMS- 14C精确定年及地球化学、物理指标的综合分析,重建了包括 8.2 ka冷期、中世纪暖期 (MWP)和小冰期 (LIA)等典型气候事件在内的全新世以来所经历的化学风化及其环境演化过程.全新世早-中期 (9.0~ 3.5 ka),岱海流域处于温暖湿润气候环境,主要环境特征表现为流域化学风化显著增强、生物生产力逐步提高、湖泊水位大幅度抬升.在 7.90~ 8.25 ka期间存在一次冷气候事件,其发生时间与来自湖沼、海洋、生物组合和极地冰芯等在内的全球环境记录基本一致,具体表现为流域化学风化减弱、湖泊生产力降低以及湖泊水位下降. 2.5 ka以来,岱海沉积物中环境指标的显著变化,表明进入气候波动更频繁的新冰期.岱海沉积物中的指标变化也展示了本世纪以来的气候增暖过程,但其化学风化强度还没有达到 MWP的程度. 相似文献
65.
国内岩石工作者对金伯利岩的分类命名不尽统一,阻碍了各金伯利岩产区的相互交流和对比。本文在分析国内现有多个分类方案的基础上,汲取其合理部分,并结合代表性产地的实际资料,提出关于对我国内生金伯利岩按“构造-结构-矿物(金云母)含量”定量分类命名的表格。 相似文献
66.
黄河三角洲滩涂资源开发利用研究 总被引:2,自引:0,他引:2
在对黄河三角洲各岸段滩涂资源特点分析的基础上,从滩涂的定义出发,结合黄河口三角洲土地资源开发利用的具体情况,对三角洲各岸段的滩涂范围进行了界定,给出了三角洲地区滩涂资源数量及其分布的研究成果。 相似文献
67.
In situ infiltration test using a reclaimed abandoned river bed: managed aquifer recharge in Shijiazhuang City,China 总被引:3,自引:1,他引:3
Managed aquifer recharge (MAR) is necessary for water resources management in arid and semiarid regions. Infiltration rate is often a decisive limiting factor in site selection for MAR. In order to avoid scale effects in the application of infiltration rate parameters, the largest in situ infiltration test in China was undertaken between August 19 and August 30, 2009 to measure the infiltration rate of the field selected for MAR in Shijiazhuang City, China. The in situ test lasted for 10 days, and about 1.82 × 107 m3 of water was introduced into the infiltration field. Groundwater level variations were monitored during the test. Monitoring showed that the infiltration rate of surface water was 1.5 m/day, which means that about 10–15 × 108 m3/a of water could be injected into the target aquifer. Also, groundwater level variations showed that the northern part of the infiltration field had a higher infiltration rate, as predicted, and the test result supplied a sound foundation for validation of the groundwater numerical simulation, which will be of benefit for future predictions of the response of the groundwater level to artificial recharge engineering. Finally, an artificial recharge plan was proposed based on the infiltration test results and the water source conditions, which would be useful for the development of MAR programs and management of local water resources. 相似文献
68.
气候变暖背景下青藏高原山地灾害及其风险分析 总被引:3,自引:0,他引:3
基于青藏高原1930-2010年山地灾害实例,分析了气候变暖对青藏高原山地灾害的影响。结果表明:在气候变暖背景下,冰湖溃决灾害增多,冰川泥石流趋于活跃,特大灾害出现频繁,灾害链生特征明显,表现出时间和空间上的延拓性,巨灾发生概率增大;在藏东南地区表现出雨热同期的气候特征,构成了利于冰川类泥石流形成的条件;波密县城位于两条泥石流危险区的建筑物占地面积由1988年0.014 km2扩展到2012年1.004 km2,人口与经济密集区与灾害高风险区重叠,加之气候变化导致的灾害危险性增加,青藏高原灾害风险显著增大。上述结果提供了气候变化对青藏高原山地灾害影响的证据,初步阐述了其影响特征,有助于山地减灾和进一步认识气候变化对山地灾害的影响机理。 相似文献
69.
Two methods are compared for estimating the shape parameters of Pareto field-size (or pool-size) distributions for petroleum
resource assessment. Both methods assume mature exploration in which most of the larger fields have been discovered. Both
methods use the sizes of larger discovered fields to estimate the numbers and sizes of smaller fields: (1) the tail-truncated
method uses a plot of field size versus size rank, and (2) the log–geometric method uses data binned in field-size classes
and the ratios of adjacent bin counts. Simulation experiments were conducted using discovered oil and gas pool-size distributions
from four petroleum systems in Alberta, Canada and using Pareto distributions generated by Monte Carlo simulation. The estimates
of the shape parameters of the Pareto distributions, calculated by both the tail-truncated and log–geometric methods, generally
stabilize where discovered pool numbers are greater than 100. However, with fewer than 100 discoveries, these estimates can
vary greatly with each new discovery. The estimated shape parameters of the tail-truncated method are more stable and larger
than those of the log–geometric method where the number of discovered pools is more than 100. Both methods, however, tend
to underestimate the shape parameter. Monte Carlo simulation was also used to create sequences of discovered pool sizes by
sampling from a Pareto distribution with a discovery process model using a defined exploration efficiency (in order to show
how biased the sampling was in favor of larger fields being discovered first). A higher (more biased) exploration efficiency
gives better estimates of the Pareto shape parameters. 相似文献
70.
Water Resources - The Kuye river watershed is a coal mining watershed in Northwest China. The study analyzed runoff change of year, high flow period and low flow period in the past 60 years based... 相似文献