全文获取类型
收费全文 | 2929篇 |
免费 | 137篇 |
国内免费 | 32篇 |
专业分类
测绘学 | 68篇 |
大气科学 | 227篇 |
地球物理 | 728篇 |
地质学 | 985篇 |
海洋学 | 262篇 |
天文学 | 442篇 |
综合类 | 14篇 |
自然地理 | 372篇 |
出版年
2024年 | 5篇 |
2023年 | 6篇 |
2022年 | 8篇 |
2021年 | 54篇 |
2020年 | 47篇 |
2019年 | 55篇 |
2018年 | 64篇 |
2017年 | 66篇 |
2016年 | 89篇 |
2015年 | 89篇 |
2014年 | 91篇 |
2013年 | 179篇 |
2012年 | 139篇 |
2011年 | 185篇 |
2010年 | 141篇 |
2009年 | 167篇 |
2008年 | 154篇 |
2007年 | 161篇 |
2006年 | 142篇 |
2005年 | 125篇 |
2004年 | 124篇 |
2003年 | 108篇 |
2002年 | 99篇 |
2001年 | 71篇 |
2000年 | 64篇 |
1999年 | 59篇 |
1998年 | 53篇 |
1997年 | 37篇 |
1996年 | 43篇 |
1995年 | 29篇 |
1994年 | 34篇 |
1993年 | 32篇 |
1992年 | 28篇 |
1991年 | 26篇 |
1990年 | 24篇 |
1989年 | 23篇 |
1988年 | 25篇 |
1987年 | 29篇 |
1986年 | 24篇 |
1985年 | 31篇 |
1984年 | 30篇 |
1983年 | 21篇 |
1982年 | 26篇 |
1981年 | 23篇 |
1980年 | 18篇 |
1979年 | 15篇 |
1978年 | 7篇 |
1977年 | 7篇 |
1974年 | 4篇 |
1971年 | 3篇 |
排序方式: 共有3098条查询结果,搜索用时 93 毫秒
241.
242.
Embedding reach-scale fluvial dynamics within the CAESAR cellular automaton landscape evolution model 总被引:2,自引:2,他引:2
We introduce a new computational model designed to simulate and investigate reach-scale alluvial dynamics within a landscape evolution model. The model is based on the cellular automaton concept, whereby the continued iteration of a series of local process ‘rules’ governs the behaviour of the entire system. The model is a modified version of the CAESAR landscape evolution model, which applies a suite of physically based rules to simulate the entrainment, transport and deposition of sediments. The CAESAR model has been altered to improve the representation of hydraulic and geomorphic processes in an alluvial environment. In-channel and overbank flow, sediment entrainment and deposition, suspended load and bed load transport, lateral erosion and bank failure have all been represented as local cellular automaton rules. Although these rules are relatively simple and straightforward, their combined and repeatedly iterated effect is such that complex, non-linear geomorphological response can be simulated within the model. Examples of such larger-scale, emergent responses include channel incision and aggradation, terrace formation, channel migration and river meandering, formation of meander cutoffs, and transitions between braided and single-thread channel patterns. In the current study, the model is illustrated on a reach of the River Teifi, near Lampeter, Wales, UK. 相似文献
243.
Brent B. Wolfe Matthew D. Falcone Ken P. Clogg-Wright Cherie L. Mongeon Yi Yi Bronwyn E. Brock Natalie A. St. Amour William A. Mark Thomas W. D. Edwards 《Journal of Paleolimnology》2007,37(2):221-231
Recent advances in sample preparation techniques and mass spectrometry have fostered more routine oxygen isotope analysis
of aquatic cellulose in lake sediment cores, a proxy for lake water oxygen isotope history. These methodological developments
have significantly increased the feasibility of incorporating this approach into high-resolution, multi-site, and multi-proxy
studies, which are frequently necessary to answer complex hydrological, hydroecological and hydroclimatic questions requiring
a paleoenvironmental perspective. Direct translation of lake sediment aquatic cellulose oxygen isotope composition into lake
water oxygen isotope composition offers appreciable opportunity for quantitative paleohydrological reconstructions, as evidenced
by studies conducted over the past 15 years that span Holocene and pre-historical timescales. 相似文献
244.
Assessment of Exploration Bias in Data-Driven Predictive Models and the Estimation of Undiscovered Resources 总被引:3,自引:0,他引:3
The spatial distribution of discovered resources may not fully mimic the distribution of all such resources, discovered and
undiscovered, because the process of discovery is biased by accessibility factors (e.g., outcrops, roads, and lakes) and by
exploration criteria. In data-driven predictive models, the use of training sites (resource occurrences) biased by exploration
criteria and accessibility does not necessarily translate to a biased predictive map. However, problems occur when evidence
layers correlate with these same exploration factors. These biases then can produce a data-driven model that predicts known
occurrences well, but poorly predicts undiscovered resources.
Statistical assessment of correlation between evidence layers and map-based exploration factors is difficult because it is
difficult to quantify the “degree of exploration.” However, if such a degree-of-exploration map can be produced, the benefits
can be enormous. Not only does it become possible to assess this correlation, but it becomes possible to predict undiscovered,
instead of discovered, resources.
Using geothermal systems in Nevada, USA, as an example, a degree-of-exploration model is created, which then is resolved into
purely explored and unexplored equivalents, each occurring within coextensive study areas. A weights-of-evidence (WofE) model
is built first without regard to the degree of exploration, and then a revised WofE model is calculated for the “explored
fraction” only. Differences in the weights between the two models provide a correlation measure between the evidence and the
degree of exploration.
The data used to build the geothermal evidence layers are perceived to be independent of degree of exploration. Nevertheless,
the evidence layers correlate with exploration because exploration has preferred the same favorable areas identified by the
evidence patterns. In this circumstance, however, the weights for the “explored” WofE model minimize this bias. Using these
revised weights, posterior probability is extrapolated into unexplored areas to estimate undiscovered deposits. 相似文献
245.
The evolving role of voluntarism in ageing rural communities 总被引:1,自引:0,他引:1
246.
247.
248.
249.
250.