全文获取类型
收费全文 | 408篇 |
免费 | 37篇 |
国内免费 | 126篇 |
专业分类
安全科学 | 8篇 |
废物处理 | 8篇 |
环保管理 | 178篇 |
综合类 | 226篇 |
基础理论 | 50篇 |
污染及防治 | 55篇 |
评价与监测 | 21篇 |
社会与环境 | 22篇 |
灾害及防治 | 3篇 |
出版年
2023年 | 6篇 |
2022年 | 9篇 |
2021年 | 14篇 |
2020年 | 8篇 |
2019年 | 20篇 |
2018年 | 17篇 |
2017年 | 18篇 |
2016年 | 26篇 |
2015年 | 32篇 |
2014年 | 26篇 |
2013年 | 27篇 |
2012年 | 32篇 |
2011年 | 41篇 |
2010年 | 27篇 |
2009年 | 27篇 |
2008年 | 22篇 |
2007年 | 13篇 |
2006年 | 37篇 |
2005年 | 16篇 |
2004年 | 22篇 |
2003年 | 17篇 |
2002年 | 14篇 |
2001年 | 20篇 |
2000年 | 12篇 |
1999年 | 5篇 |
1998年 | 10篇 |
1997年 | 9篇 |
1996年 | 4篇 |
1995年 | 7篇 |
1994年 | 5篇 |
1993年 | 1篇 |
1992年 | 3篇 |
1991年 | 3篇 |
1990年 | 2篇 |
1988年 | 5篇 |
1987年 | 1篇 |
1986年 | 2篇 |
1985年 | 3篇 |
1984年 | 1篇 |
1982年 | 2篇 |
1981年 | 1篇 |
1980年 | 2篇 |
1977年 | 1篇 |
1975年 | 1篇 |
排序方式: 共有571条查询结果,搜索用时 15 毫秒
61.
潜流人工湿地系统停留时间分布与N、P浓度空间变化 总被引:2,自引:0,他引:2
通过人工湿地小试装置,研究了风车草和香蒲水平潜流人工湿地处理富营养化养殖水体过程中水力停留时间分布(RTD)特征和系统内N、P浓度空间变化规律.结果表明,供试的香蒲潜流湿地和风车草潜流湿地系统RTD曲线特征值σ2分别为0.324 6和0.410 8,表明水流流态介于推流与混合流之间,风车草潜流湿地系统RTD曲线较香蒲潜流湿地平滑,水流混合流动程度较弱. 2种植物类型湿地床体总氮(TN)和氨氮(NH+4-N)浓度在垂直方向上的分层现象明显,尤其在湿地床体前端;TN浓度随着取样点深度增加而上升,而NH+4-N浓度则以中层取样点为最低;对于总磷(TP)和正磷酸盐(PO3-4-P)浓度, 2种植物类型湿地系统内均表现为随取样点深度增加而上升,但这种差异随沿程而降低. 与香蒲湿地相比较,风车草潜流湿地系统N、P浓度分层现象更为明显.风车草湿地系统后端各层取样点TN和TP平均浓度较香蒲湿地系统分别下降了19.8%和12.3%,说明风车草潜流湿地系统对富营养化养殖水体中氮、磷的去除效果优于香蒲湿地. 相似文献
62.
土地利用变化对湿地景观连通性的影响及连通性优化效应——以江苏盐城海滨湿地为例 总被引:6,自引:0,他引:6
土地利用与土地覆盖变化对湿地景观的结构和功能产生深刻的影响。选择江苏盐城海滨地区为研究对象,应用遥感和地理信息系统技术,分析20年来土地利用变化对湿地景观连通性的影响,并以2007年湿地景观生态系统服务功能为基础,采用阻力面模型探讨湿地景观连通性优化途径及其效应。结果显示:①1987—2007年间,盐城海滨区域土地利用结构变化显著。其中耕地面积比重由36.72%上升为46.17%,自然湿地持续减少,面积由44.4%减为26.01%,人工湿地持续增加,面积由9.96%上升为18.72%;②随着区域人类土地利用活动的加强,光滩、碱蓬沼泽和芦苇沼泽的空间连通性降低,区域土地利用导致湿地景观之间生态流阻隔,景观生态服务功能减弱;③2007年湿地景观生态功能强度空间差异显著,以累积耗费距离面、生态源地、耗费路径为依据,对湿地景观连通路径优化结果表明,废黄河口和大丰港附近等关键区域对景观连通性和生态流影响最大,是景观生态节点优化的首要对象;④加强连通路径的关键区域优化、提高景观连通度是实现景观优化的关键。 相似文献
63.
设计了垂直流+水平流、水平流+垂直流、单一水平、单一垂直等4组不同结构的人工湿地组合,研究其对生活污水的净化效果。结果表明:4组人工湿地对CODCr,TP的去除率分别达到80%,70%左右;对TN的去除,垂直+水平单元去除率最高,为44.30%。 相似文献
64.
Anna M. Jalowska Yongping Yuan 《Journal of the American Water Resources Association》2019,55(1):209-227
Worldwide studies show 80%–90% of all sediments eroded from watersheds is trapped within river networks such as reservoirs, ponds, and wetlands. To represent the impact of impoundments on sediment routing in watershed modeling, Soil and Water Assessment Tool (SWAT) developers recommend to model reservoirs, ponds, and wetlands using impoundment tools (ITs). This study evaluates performance of SWAT ITs in the modeling of a small, agricultural watershed dominated by lakes and wetlands. The study demonstrates how to incorporate impoundments into the SWAT model, and discusses and evaluates involved parameters. The study then recommends an appropriate calibration sequence, i.e., landscape parameters calibration, followed by pond/wetlands calibration, then channel parameter calibrations, and lastly, reservoir parameter calibration. Results of this study demonstrate not following SWAT recommendation regarding modeling water land use as an impoundment depreciates SWAT performance, and may lead to misplaced calibration efforts and model over‐calibration. Further, the chosen method to model impoundments’ outflow significantly impacts sediment loads in the watershed, while streamflow simulation is not very sensitive. This study also allowed calculation of mass accumulation rates in modeled impoundments where the annual mass accumulation rate in wetlands (2.3 T/ha/yr) was 39% higher than mass accumulation rate in reservoirs (1.4 T/ha/yr). 相似文献
65.
David I.S. Green Samuel M. McDeid William G. Crumpton 《Journal of the American Water Resources Association》2019,55(3):543-558
We present estimates of the volumetric storage capacities of currently drained upland depressions and catchment depressional specific storage and runoff storage indices for the Des Moines Lobe of Iowa (DML‐IA) subregion of the Prairie Pothole Region of North America. Storage capacities were determined using hydrologically enforced Light Detection and Ranging‐derived digital elevation models, and a unique geoprocessing algorithm. Depressional specific storage was estimated for each 12‐digit Hydrologic Unit Code (HUC12) watershed in the region from total catchment‐specific depressional storage volume and catchment area. Runoff storage indices were calculated using catchment depressional specific storage values and estimates of the amount of rainfall likely to fall within each watershed during sub‐annual and 1‐, 2‐, 5‐, and 10‐year 24‐h events. The 173,171 identified drained depressions in the DML‐IA can store up to 903.5 Mm3 of runoff. Most of this capacity is in depressions located in the north of the region. Specific storage varies from nearly 109 mm in the younger landscapes to <10 mm in older more eroded areas. For 95% of the HUC12 watersheds comprising the region, depressional storage will likely be exhausted by rainfall‐derived runoff in excess of a 1‐year 24‐h event. Rainfall amounts greater than a 5‐year 24‐h event will exceed all available depressional storage. Therefore, the capacity of drained depressions in the DML‐IA to mitigate flooding resulting from infrequent, but large, storm events is limited. 相似文献
66.
为了明确北方大规模人工湿地在冬季对TCS(三氯生)的去除效果,在山东省境内4个典型的大规模人工湿地(即武河人工湿地、大沙河人工湿地、新薛河人工湿地和洸府河人工湿地)内于冬季(2013年12月—2014年1月)进行取样,以超高效液相色谱串联质谱法测定人工湿地进出水中ρ(TCS),并分析不同湿地对TCS的去除效果. 结果表明:TCS在4个人工湿地系统进出水中均有检出,由于各人工湿地系统均承接当地污水处理厂尾水,冬季进水中ρ(TCS)偏高,为(800.81±83.37)~(1 151.00±47.13) ng/L,并以武河人工湿地为最高. 虽然人工湿地对TCS的去除率达22.44%~78.82%,但经由人工湿地处理后出水中仍含有较高浓度的TCS残留,经由人工湿地出水进入下游水体的TCS日释放量仍较高,其中洸府河人工湿地出水中高达92.60 g. 因此,冬季各人工湿地对TCS的去除效果在低温影响下有所降低,并且对下游水体和人类健康的威胁不容忽视. 相似文献
67.
Physical and Chemical Connectivity of Streams and Riparian Wetlands to Downstream Waters: A Synthesis
下载免费PDF全文
![点击此处可从《Journal of the American Water Resources Association》网站下载免费的PDF全文](/ch/ext_images/free.gif)
Ken M. Fritz Kate A. Schofield Laurie C. Alexander Michael G. McManus Heather E. Golden Charles R. Lane William G. Kepner Stephen D. LeDuc Julie E. DeMeester Amina I. Pollard 《Journal of the American Water Resources Association》2018,54(2):323-345
Streams, riparian areas, floodplains, alluvial aquifers, and downstream waters (e.g., large rivers, lakes, and oceans) are interconnected by longitudinal, lateral, and vertical fluxes of water, other materials, and energy. Collectively, these interconnected waters are called fluvial hydrosystems. Physical and chemical connectivity within fluvial hydrosystems is created by the transport of nonliving materials (e.g., water, sediment, nutrients, and contaminants) which either do or do not chemically change (chemical and physical connections, respectively). A substantial body of evidence unequivocally demonstrates physical and chemical connectivity between streams and riparian wetlands and downstream waters. Streams and riparian wetlands are structurally connected to downstream waters through the network of continuous channels and floodplain form that make these systems physically contiguous, and the very existence of these structures provides strong geomorphologic evidence for connectivity. Functional connections between streams and riparian wetlands and their downstream waters vary geographically and over time, based on proximity, relative size, environmental setting, material disparity, and intervening units. Because of the complexity and dynamic nature of connections among fluvial hydrosystem units, a complete accounting of the physical and chemical connections and their consequences to downstream waters should aggregate over multiple years to decades. 相似文献
68.
69.
70.