全文获取类型
收费全文 | 8607篇 |
免费 | 670篇 |
国内免费 | 1873篇 |
专业分类
安全科学 | 473篇 |
废物处理 | 30篇 |
环保管理 | 1457篇 |
综合类 | 5542篇 |
基础理论 | 850篇 |
环境理论 | 4篇 |
污染及防治 | 331篇 |
评价与监测 | 616篇 |
社会与环境 | 1466篇 |
灾害及防治 | 381篇 |
出版年
2024年 | 56篇 |
2023年 | 145篇 |
2022年 | 308篇 |
2021年 | 313篇 |
2020年 | 314篇 |
2019年 | 299篇 |
2018年 | 285篇 |
2017年 | 353篇 |
2016年 | 445篇 |
2015年 | 499篇 |
2014年 | 396篇 |
2013年 | 513篇 |
2012年 | 678篇 |
2011年 | 708篇 |
2010年 | 488篇 |
2009年 | 473篇 |
2008年 | 438篇 |
2007年 | 600篇 |
2006年 | 599篇 |
2005年 | 512篇 |
2004年 | 391篇 |
2003年 | 374篇 |
2002年 | 318篇 |
2001年 | 240篇 |
2000年 | 242篇 |
1999年 | 199篇 |
1998年 | 134篇 |
1997年 | 128篇 |
1996年 | 113篇 |
1995年 | 99篇 |
1994年 | 87篇 |
1993年 | 74篇 |
1992年 | 57篇 |
1991年 | 45篇 |
1990年 | 41篇 |
1989年 | 14篇 |
1988年 | 21篇 |
1987年 | 13篇 |
1986年 | 11篇 |
1985年 | 10篇 |
1984年 | 6篇 |
1983年 | 7篇 |
1982年 | 13篇 |
1981年 | 13篇 |
1980年 | 15篇 |
1979年 | 16篇 |
1978年 | 9篇 |
1973年 | 6篇 |
1972年 | 9篇 |
1971年 | 8篇 |
排序方式: 共有10000条查询结果,搜索用时 328 毫秒
761.
利用极端降水量集中度和集中期讨论三峡库区汛期极端降水量的非均匀性分布特征。结果表明: 三峡库区极端降水量空间分布表现为西南部和东北部地区相对较少,中部、东南部相对较多。库区汛期极端降水集中度和集中期的空间差异不大,集中程度总体较差,东北部和西部地区极端降水相对集中,中部相对分散。库区极端降水主要集中在6月底和7月上中旬,东北部和西部偏西地区集中期相对较晚,中部地区集中期相对较早。库区汛期极端降水量的分配状况与同期极端降水量存在较好的关系,即极端降水量越少,则极端降水量越集中、集中期越早;反之极端降水量越多,则极端降水量越分散、集中期越晚,尤其是在库区东北部地区最为显著。三峡库区蓄水后极端降水集中程度在空间上一致性较好,表现为蓄水后更为分散;极端降水量和集中期则在空间上差异显著,大致表现为蓄水后东北部极端降水增加并延迟;西南部极端降水减少并提前 相似文献
762.
三峡工程蓄水运用期库区干流水质分析 总被引:6,自引:0,他引:6
分析了三峡库区蓄水前后(1998~2009年)干流水质的变化及原因。结果表明,同蓄水前相比,蓄水后库区干流水质变好,库区干流断面月度达标率均值由蓄水前的623%变为蓄水后的783%,库区干流超标污染物主要为高锰酸盐指数、总磷、铅等。蓄水后水质时空分布出现新的特点,近坝水体悬浮物、浑样高锰酸盐指数、总磷、铅等可吸附污染物浓度显著降低。蓄水后年内悬浮物及浑样高锰酸盐指数、总磷和铅浓度仍然是丰水期>平、枯水期,但近坝水体不同水期间浓度差别比蓄水前明显减小。蓄水后,库区干流浑样高锰酸盐指数、总磷、铅浓度整体上表现为从库尾至库首沿程下降,尤以丰水期沿程下降最为突出。浑样高锰酸盐指数、总磷、铅浓度以上变化特征主要缘于库区水位抬高后,流速减小导致的澄清作用,即高锰酸盐指数所代表污染物、磷、铅等随泥沙发生了不同程度的沉降。蓄水前后清样高锰酸盐指数和总磷未发生明显变化,156 m蓄水后至今,清样铅浓度明显低于蓄水前。 相似文献
763.
764.
765.
为了评价新民柳河水源地的供水安全,简要介绍水环境健康风险评价基本方法的基础上,建立了水环境健康风险评价模式.研究结果表明:①柳河水源地地面水基因毒物质为优先控制污染物;而地下水应着力控制躯体毒物质.②对于基因毒物质,监测断面优先控制污染物为As和Cr;而对于躯体毒物质,所有监测断面的优先控制污染物均为氨.③在所有监测断面中,柳河上断面等6处有毒污染物所致健康危害的个人年总风险数量级为10-5-10-4.在日后的管理过程中,应对这6处加大治理力度.④目前环境健康风险评价还没有包括在常规环境评价工作中,建议在今后的评价工作中应该逐步开展这方面的工作,以提高供水安全. 相似文献
766.
767.
We examined the influence of several hydrological and meteorological parameters on the migratory movements of ayu Plecoglossus altivelis altivelis in central Japan. When comprehensively evaluating rivers and ayu behaviour on a catchment scale, the subjects of analysis typically include human activities and hydrological and meteorological phenomena. However, limiting analyses to such factors may be too restrictive when human activities are being conducted. Accordingly, we incorporated a biological viewpoint into the evaluation method, analysing hydrological data (river discharge, river water temperature, sea water temperature) to determine watershed characteristics and examining the relationship between these characteristics and the habitat conditions of ayu. Then we constructed a numerical model for ayu migratory runs that incorporated ayu ecology and watershed characteristics. Analyses of ayu movements from a lower estuarine dam demonstrated that downstream displacements were associated with high water flows of more than 200 m3 s−1 at the beginning of summer. We conclude that it is important to consider the effects of environmental parameters on the movements of different fish species to understand the causes of spatial variation in fish distribution in lowland rivers. 相似文献
768.
David M. Meko Matthew D. Therrell Christopher H. Baisan Malcolm K. Hughes 《Journal of the American Water Resources Association》2001,37(4):1029-1039
ABSTRACT: A time series of annual flow of the Sacramento River, California, is reconstructed to A.D. 869 from tree rings for a long‐term perspective on hydrologic drought. Reconstructions derived by principal components regression of flow on time‐varying subsets of tree‐ring chronologies account for 64 to 81 percent of the flow variance in the 1906 to 1977 calibration period. A Monte Carlo analysis of reconstructed n‐year running means indicates that the gaged record contains examples of drought extremes for averaging periods of perhaps = 6 to 10 years, but not for longer and shorter averaging periods. For example, the estimated probability approaches 1.0 that the flow in A.D. 1580 was lower than the lowest single‐year gaged flow. The tree‐ring record also suggests that persistently high or low flows over 50‐year periods characterize some parts of the long‐term flow history. The results should contribute to sensible water resources planning for the Sacramento Basin and to the methodology of incorporating tree‐ring data in the assessment of the probability of hydrologic drought. 相似文献
769.
Stephen T. Gray Jeffrey J. Lukas Connie A. Woodhouse 《Journal of the American Water Resources Association》2011,47(4):702-712
Gray, Stephen T., Jeffrey J. Lukas, and Connie A. Woodhouse, 2011. Millennial‐Length Records of Streamflow From Three Major Upper Colorado River Tributaries. Journal of the American Water Resources Association (JAWRA) 47(4):702‐712. DOI: 10.1111/j.1752‐1688.2011.00535.x Abstract: Drought, climate change, and shifting consumptive use are prompting a widespread reassessment of water availability in the Upper Colorado River basin. Here, we present millennial‐length records of water year (October‐September) streamflow for key Upper Colorado tributaries: the White, Yampa, and Little Snake Rivers. Based on tree rings, these records represent the first paleohydrological reconstructions from these subbasins to overlap with a series of Medieval droughts (∼ad 800 to 1300). The reconstructions show marked interannual variability imbedded in nonstationary behavior over decadal to multidecadal time scales. These reconstructions suggest that, even in a millennial context, gaged flows from a handful of years (e.g., 1977 and 2002) were extremely dry. However, droughts of much greater duration and magnitude than any in the instrumental record were regular features prior to 1900. Likewise these reconstructions point to the unusual wetness of the gage period, and the potential for recent observations to paint an overly optimistic picture of regional water supplies. The future of the Upper Colorado River will be determined by a combination of inherent hydroclimatic variability and a broad range of human‐induced changes. It is then essential that regional water managers, water users, and policy makers alike consider a broader range of hydroclimatic scenarios than is offered by the gage record alone. 相似文献
770.
Disturbance regimes,resilience, and recovery of animal communities and habitats in lotic ecosystems 总被引:6,自引:0,他引:6
Disturbance regime is a critical organizing feature of stream communities and ecosystems. The position of a given reach in
the river basin and the sediment type within that reach are two key determinants of the frequency and intensity of flow-induced
disturbances. We distinguish between predictable and unpredictable events and suggest that predictable discharge events are
not disturbances.
We relate the dynamics of recovery from disturbance (i.e., resilience) to disturbance regime (i.e., the disturbance history
of the site). The most frequently and predictably disturbed sites can be expected to demonstrate the highest resilience.
Spatial scale is an important dimension of community structure, dynamics, and recovery from disturbance. We compare the effects
on small patches (⩽1 m2) to the effects of large reaches at the river basin level. At small scales, sediment movements and scour are major factors
affecting the distribution of populations of aquatic insects or algae. At larger scales, we must deal with channel formation,
bank erosion, and interactions with the riparian zone that will affect all taxa and processes.
Our understanding of stream ecosystem recovery rests on our grasp of the historical, spatial, and temporal background of contemporary
disturbance events. 相似文献