全文获取类型
收费全文 | 1063篇 |
免费 | 205篇 |
国内免费 | 202篇 |
专业分类
测绘学 | 5篇 |
大气科学 | 1篇 |
地球物理 | 392篇 |
地质学 | 979篇 |
海洋学 | 16篇 |
综合类 | 48篇 |
自然地理 | 29篇 |
出版年
2024年 | 4篇 |
2023年 | 4篇 |
2022年 | 22篇 |
2021年 | 31篇 |
2020年 | 29篇 |
2019年 | 38篇 |
2018年 | 54篇 |
2017年 | 39篇 |
2016年 | 37篇 |
2015年 | 46篇 |
2014年 | 64篇 |
2013年 | 114篇 |
2012年 | 53篇 |
2011年 | 59篇 |
2010年 | 51篇 |
2009年 | 75篇 |
2008年 | 100篇 |
2007年 | 83篇 |
2006年 | 79篇 |
2005年 | 71篇 |
2004年 | 63篇 |
2003年 | 61篇 |
2002年 | 32篇 |
2001年 | 36篇 |
2000年 | 45篇 |
1999年 | 28篇 |
1998年 | 29篇 |
1997年 | 29篇 |
1996年 | 17篇 |
1995年 | 13篇 |
1994年 | 13篇 |
1993年 | 16篇 |
1992年 | 15篇 |
1991年 | 5篇 |
1990年 | 4篇 |
1989年 | 5篇 |
1988年 | 1篇 |
1987年 | 1篇 |
1985年 | 1篇 |
1982年 | 1篇 |
1978年 | 1篇 |
1973年 | 1篇 |
排序方式: 共有1470条查询结果,搜索用时 15 毫秒
81.
Branka Trček 《Environmental Geology》2007,51(5):761-765
The role of an epikarst zone in the karst aquifer hydraulic behaviour was brought into focus in our studies referring to the
catchment area of the Hubelj spring (SW Slovenia). This study points out the significance of effects of the fast preferential
flow—epiflow, which is the main factor controlling solute/contaminant transport towards the aquifer saturated zone. The so-called
epikarstic hypothesis is verified on the basis of the most significant research results that are supported by the most important
findings from the literature. 相似文献
82.
地下水化学动力学基本理论在矿井水文地质中的应用 总被引:2,自引:0,他引:2
根据西峪煤矿水化学及相关水文地质资料,运用地下水化学动力学的基本理论和方法,对西峪煤矿奥陶系峰峰组岩溶含水层水文地质条件进行了定量评价,从而划分出了含水层的强、弱径流带,为煤矿的安全生产提供了依据。 相似文献
83.
84.
85.
通过对山西榆次地裂缝及墙体裂缝的动态监测,发现如下特征:地裂缝总体趋势为增大,年速率小于等于1mm/a。东部地裂缝带地裂平均速率为0.6mm/a,且大于西部地裂缝带,地裂有向东南方向(榆次市区)扩展的态势;从曲线形态看,无论是地面测点还是建筑物上的测点,都不同程度地受气温变化和降水的干扰。裂缝与温度的变化呈负相关,与降水的变化呈正相关。从地裂的分布形状、区域形变场特征及新构造运动的角度看,附近的断裂活动与地裂的发展似有一定的关系。 相似文献
86.
87.
通过对淮北市地质、水文地质条件的综合分析 ,建立了淮北市双含水层系统水文地质概念模型。引入准三维流数学模型进行地下水动态预报及建立地下水管理模型。用线性规划模型提出淮北市地下水资源的最佳管理方案。最后提出开展地下水回灌研究、建立岩溶含水层地下水库、限制发展耗水型工业及用法律和经济手段管理水资源开发等建议 相似文献
88.
A model of the early evolution of karst aquifers in limestone in the dimensions of length and depth 总被引:5,自引:0,他引:5
《Journal of Hydrology》2001,240(3-4):206-224
A new model of the early evolution of limestone karst aquifers in the dimensions of length and depth is presented. In its initial state the aquifer consists of a rock massive with evenly spaced fractures of about 50 μm aperture widths with an hydraulic conductivity of 10−7 ms−1. In addition to this a coarser network of prominent fractures with aperture widths of several 100 μm is also present. Boundary conditions of constant recharge 450 mm/year, or constant head from the input of allogenic streams are imposed. First the position of the water table in the aquifer is calculated, then dissolutional widening during a time step in all the fractures below the water table is found by use of the well-known nonlinear dissolution kinetics of limestone. This is iterated and the position of the water table as well as the fracture widths are found as a function of time. In the case of constant recharge to a karst plateau, the water table in any case drops to base level and conduits there propagate from the spring headwards. If constant head conditions are valid the position of the water table remains almost stable and conduits propagate along the water table from the input towards the spring. There is competition between conduit evolution along prominent fractures and along tight fissures close to the water table. In any case under constant head conditions one of these pathways wins, and early karst evolution is terminated by a breakthrough event with an explosive increase of the flow through the aquifer until constant head conditions break down. Depending on the boundary conditions of constant head or constant recharge or a combination of both it is possible to describe models of cave genesis, which have been derived from field evidence, such as the water table models of Swinnerton and Rhoades as well as the four-state model by Ford and Ewers (Can. J. Earth Sci., 15 (1978) 1783). 相似文献
89.
90.
Sedimentary rocks have structures on all length scales from the millimeter to the kilometer. These structures are generally associated with variations in rock permeability. These need to be modeled if we are to make predictions about fluid flow through the rock. However, existing computers are not powerful enough for us to be able to represent all scales of heterogeneity explicitly in our fluid flow models—hence, we need to upscale. Small cell renormalization is a fast method for upscaling permeability, derived from an analogue circuit of resistors. However, it assumes that the small scale permeability distribution is known. In practice, this is unlikely. The only information available about small scale properties is either qualitative, derived from the depositional setting of the reservoir, or local to the wells as a result of coring or logging. The influence of small scale uncertainty on large scale properties is usually modelled by the Monte Carlo method. This is time-consuming and inaccurate if not enough realisations are used. This paper describes a new implementation of renormalization, which enables the direct upscaling of uncertain small-scale permeabilities to produce the statistical properties of the equivalent coarse grid. This is achieved by using a perturbation expansion of the resistor-derived equation. The method is verified by comparison with numerical simulations using the Monte Carlo method. The prediction of expected large-scale permeability and its standard deviation are shown to be accurate for small cell standard deviations of up to 40% of the mean cell value, using just the first nonzero term of the perturbation expansion. Inclusion of higher order terms allows larger standard deviations to be modeled accurately. Evaluation of cross-terms allows correlations of actual cell values, over and above the background structure of mean cell values. The perturbation method is significantly faster than conventional Monte Carlo simulation. It needs just two calculations whereas the Monte Carlo method needs many thousands of realisations to be generated and renormalized to converge. This results in significant savings in computer time. 相似文献