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31.
Doan Van Binh Sameh A. Kantoush Tetsuya Sumi Nguyen Phuong Mai Trieu Anh Ngoc La Vinh Trung Tran Dang An 《水文研究》2021,35(2):e14030
The hydrogeomorphology of the Vietnamese Mekong Delta (VMD) has been significantly altered by natural and anthropogenic drivers. In this study, the spatiotemporal changes of the flow regime were examined by analysing the long-term daily, monthly, annual and extreme discharges and water levels from 1980 to 2018, supported by further investigation of the long-term annual sediment load (from the 1960s to 2015), river bathymetric data (in 1998, 2014 and 2017) and daily salinity concentration (from the 1990s to 2015) using various statistical methods and a coupled numerical model. Then, the effects of riverbed incision on the hydrology were investigated. The results show that the dry season discharge (i.e., in March–June) of the Tien River increased by up to 23% from the predam period (1980–1992) to the postdam period (1993–2018) but that the dry season water level at My Thuan decreased by up to −46%. The annual mean and monthly water levels in June at Tan Chau and in January and June–October at My Thuan in the Tien River decreased statistically, even though the respective discharges increased significantly. These decreased water levels instead of the increased discharges were attributed to the accelerated riverbed incision upstream from My Thuan, which increased by more than three times, from a mean rate of −0.16 m/year (−16.7 Mm3/year) in 1998–2014 to −0.5 m/year (−52.5 Mm3/year) in 2014–2017. This accelerated riverbed incision was likely caused by the reduction in the sediment load of the VMD (from 166.7 Mt/year in the predam period to 57.6 Mt/year in the postdam period) and increase in sand mining (from 3.9 Mm3 in 2012 to 13.43 Mm3 in 2018). Collectively, the decreased dry season water level in the Tien River is likely one of the main causes of the enhanced salinity intrusion. 相似文献
32.
江峰 《中国地质灾害与防治学报》2009,20(4):36-40
本文以南靖县帮科泥石流防治工程设计工作为例,选取了影响该泥石流形成的10项因子,利用模糊数学综合评判法对该泥石流危险程度进行了评价,为福建省泥石流预测预报及防治提供了定量的数学分析方法,有利于福建省科学防灾工作的进一步开展。此外,本文还对帮科泥石流防治工程中拦挡坝的设计方法进行了初步探讨,明确提出设计中坝体的稳定性演算可以简化为抗滑稳定演算等三个注意事项,并针对福建省的气候、土壤条件,提供了泥石流生物治理措施中的几种优势树种及其基本种植方案。相信本文对福建省其他泥石流防治工程设计具有借鉴意义。 相似文献
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《国际泥沙研究》2020,35(5):431-443
In recent years, the damage caused to human settlements in Japan by large woody debris (LWD) has been increasing. For example, the 2013 Izu Oshima typhoon resulted in a large number of fatalities and missing persons, and the Kagoshima Typhoon Disaster and Northern Kyusyu torrential downpour caused vast infrastructure damage due to the associated LWD. Current countermeasures for preventing LWD are insufficient to maintain the safety of residential areas. One type of protective barrier, the open sabo dam, has been constructed in Japan during the past 30 years. The primary function of open sabo dams is to block the flow of boulders, thereby also reducing sediment flow by reducing the gap size. However, because Japanese open sabo dams are designed specifically for boulder-trapping, the ability of these dams to trap LWD remains uncertain. In particular, many problems have been reported with respect to sediment trapping by driftwood with roots in an open sabo dam setting. The objective of this study was to examine the trapping efficiency of open sabo dams for LWD and sediment. The experimental approach clarified the influence of driftwood, without and with roots, on sediment trapping for a straight-channel flume. The flexible roots of the driftwood were shown to have a significant effect on the sediment trapping efficiency of the dam. 相似文献
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由于可液化砂质土应力-应变特性模拟的复杂性及数值计算的不稳定性,深厚砂质覆盖层土坝的弹塑性地震反应分析是土坝抗震研究中的一个尚未完全解决的课题。采用u-p完全耦合的饱和多孔介质有限元分析方法和砂土多重机构弹塑性模型,对遭受M6.7级地震的国外某深厚砂质覆盖层土坝进行弹塑性地震反应分析,研究了坝体和地基的动力反应特性及其超静孔隙水压力产生、扩散和消散的变化规律。结果表明:计算得到的坝体加速度和永久变形与实测值存在一定的差异,但基本上反映了坝体加速度与永久变形的实际分布情况,从而说明采用的本构模型和计算方法具有一定的精度;由于坝体和坝基的超静孔隙水压力较小,且坝体永久变形不大,可以不对坝体和坝基进行加固处理;坝趾附近浅层地基的超静孔隙水压力较大,有可能发生液化,因此,须采取相应的抗液化加固措施。 相似文献
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Gregory B. Baecher 《Georisk: Assessment and Management of Risk for Engineered Systems and Geohazards》2016,10(2):92-108
The character and importance of uncertainty in dam safety risk analysis drives how risk assessments are used in practice. The current interpretation of uncertainty is that, in addition to the aleatory risk which arises from presumed uncertainty in the world, it comprises the epistemic aspects of irresolution in a model or forecast, specifically model and parameter uncertainty. This is true in part but it is not all there is to uncertainty in risk analysis. The physics of hazards and of failure may be poorly understood, which goes beyond uncertainty in its conventional sense. There may be alternative scenarios of future conditions, for example non-stationarity in the environment, which cannot easily be forecast. There may also be deep uncertainties of the type associated with climate change. These are situations in which analysts do not know or do not agree on the system characterisation relating actions to consequences or on the probability distributions for key parameters. All of these facets are part of the uncertainty in risk analysis with which we must deal. 相似文献
40.
本文以上犹江水电站左岸地下水渗漏检测及分析为例,介绍以伪随机流场法、综合水量均衡法、水质和析出物化学分析法等相结合的渗漏检测与分析的方法技术,检测的结果与已有的工程地质资料以及水工观测资料是一致的.该方法技术体系不仅能查明水库渗水来源,还对渗漏通道、渗漏原因进行推断分析,避免以往单一方法的片面性,为检测分析水库坝基的渗漏提供了一种新的思路. 相似文献