全文获取类型
收费全文 | 458篇 |
免费 | 31篇 |
国内免费 | 137篇 |
专业分类
安全科学 | 19篇 |
废物处理 | 7篇 |
环保管理 | 38篇 |
综合类 | 274篇 |
基础理论 | 160篇 |
污染及防治 | 30篇 |
评价与监测 | 90篇 |
社会与环境 | 7篇 |
灾害及防治 | 1篇 |
出版年
2024年 | 2篇 |
2023年 | 5篇 |
2022年 | 9篇 |
2021年 | 12篇 |
2020年 | 10篇 |
2019年 | 11篇 |
2018年 | 17篇 |
2017年 | 10篇 |
2016年 | 23篇 |
2015年 | 25篇 |
2014年 | 20篇 |
2013年 | 60篇 |
2012年 | 27篇 |
2011年 | 24篇 |
2010年 | 19篇 |
2009年 | 12篇 |
2008年 | 15篇 |
2007年 | 16篇 |
2006年 | 45篇 |
2005年 | 29篇 |
2004年 | 24篇 |
2003年 | 29篇 |
2002年 | 19篇 |
2001年 | 19篇 |
2000年 | 14篇 |
1999年 | 17篇 |
1998年 | 20篇 |
1997年 | 14篇 |
1996年 | 15篇 |
1995年 | 7篇 |
1994年 | 11篇 |
1993年 | 8篇 |
1992年 | 6篇 |
1991年 | 7篇 |
1990年 | 10篇 |
1989年 | 4篇 |
1988年 | 1篇 |
1986年 | 3篇 |
1984年 | 1篇 |
1983年 | 1篇 |
1982年 | 2篇 |
1972年 | 2篇 |
1971年 | 1篇 |
排序方式: 共有626条查询结果,搜索用时 62 毫秒
41.
42.
新化矿区煤矸石中微量元素赋存形态及浸出特征 总被引:1,自引:0,他引:1
利用BCR连续提取法和浸泡实验,对贵州省新化煤矿区不同风化程度的煤矸石中微量元素As、Cd、V、Zn、Co、Cr、Cu、Ni、Pb的赋存形态及浸出浓度进行研究。赋存形态研究结果表明:在煤矸石中As和Cd元素主要以酸溶态、可还原态和可氧化态形式赋存,而其他微量元素V、Zn、Co、Cr、Cu、Ni、Pb主要以残渣态形式赋存;除了V元素的赋存形态含量百分比不受煤矸石风化程度影响外,其它微量元素的赋存形态的含量百分比均会受到煤矸石风化程度的影响。煤矸石的浸出实验表明:浸泡时间是影响煤矸石中微量元素释放的一个重要因素;在浸泡过程中,大部分微量元素在浸泡前期的浸出浓度受煤矸石风化程度的影响,Zn和Cu元素则是在整个浸泡过程的浸出浓度均受到煤矸石风化程度的影响;不同粒径大小的煤矸石在浸泡过程中,除微量元素As和Co的浸出浓度不受煤矸石粒径大小的影响,其他微量元素在浸泡前期和中期的浸出浓度均与煤矸石的粒径大小呈反比。 相似文献
43.
N,N-双(二硫代羧基)乙二胺对微量络合镍的深度脱除特性研究 总被引:2,自引:1,他引:1
以柠檬酸镍(CA-Ni)、酒石酸镍(TA-Ni)、焦磷酸镍(SP-Ni)3种低浓度模拟络合镍废水为研究对象,选用自制的重金属捕集剂N,N-双(二硫代羧基)乙二胺(EDTC),对废水中的Ni进行深度脱除.重点研究了EDTC投加量、初始p H、反应时间对Ni去除效果的影响及螯合沉淀物的沉淀性能和溶出特性,同时分析了EDTC去除络合Ni的机理.研究结果表明,处理初始浓度5 mg·L~(-1)的CA-Ni、TA-Ni、SP-Ni,p H为4~8,EDTC最佳投加量分别为60 mg·L~(-1)、55 mg·L~(-1)和70 mg·L~(-1),PAM(聚丙烯酰胺)为1 mg·L~(-1),反应时间2 min,Ni的出水浓度均低于0.05mg·L~(-1),去除率达99%以上.螯合沉淀物沉降性能好且在弱酸弱碱条件下能稳定存在.红外光谱图和元素分析结果表明:EDTC与Ni发生螯合反应,即EDTC直接脱除络合镍中的Ni2+,并与Ni2+生成更稳定的螯合产物EDTC-Ni,进而有效地去除废水中Ni. 相似文献
44.
45.
Sediment cores were collected from two remote subalpine lakes: the rather shallow (1.5 m) Little Ghost Lake at 2040 m elevation and the deeper, Great Ghost Lake (40 m) at 2150 m elevation. Different early diagenesis of metals were observed. the seasonally anoxic hypolimnion drives the annual iron redox cycle and causes the remobilization of metals in the mobile fractions of sediments in the Great Ghost Lake. These result in the redistribution of metals in the mobile fractions of sediment and poor correlation between metal concentrations. in the Little Ghost Lake, the shallow water column is always oxic with less change of metals in the mobile fractions of sediments. As a result, most metals have strong positive correlations with each other.
The distributions of metal/Al ratios, total metal contents and acid-leached metal concentrations in the near-surface sediments of these two lakes suggest that the anthropogenic inputs from the atmospheric fallouts in recent decades are one of the major factors affecting the distributions of metals such as cadmium, lead and, to a lessor extent, zinc. the Pb-206/Pb-207 ratios confirm the anthropogenic lead input in these surface sediments. 相似文献
The distributions of metal/Al ratios, total metal contents and acid-leached metal concentrations in the near-surface sediments of these two lakes suggest that the anthropogenic inputs from the atmospheric fallouts in recent decades are one of the major factors affecting the distributions of metals such as cadmium, lead and, to a lessor extent, zinc. the Pb-206/Pb-207 ratios confirm the anthropogenic lead input in these surface sediments. 相似文献
46.
The National Oceanic and Atmospheric Administration's (NOAA) National Status and Trends (NS&T) Programme has analyzed samples of surface sediment collected at almost 300 coastal and estuarine sites throughout the United States since 1984. the overall distributions for concentrations of each element are approximately lognormal allowing a definition of geometric means and of “high” concentrations as those exceeding the mean plus one standard deviation of the lognormal distribution. Those mean and “high” concentrations should be useful for comparing the NS&T data set and with other reports on sediment contamination. A world-wide data set, constructed from data in the literature, was summarized in an identical manner. It was found, after excluding locally extreme values, that the NS&T and world-wide data sets yielded very similar mean and “high” concentrations for Cu, Ni, Pb and Zn. Chromium was the sole element showing higher summary statistics in the NS&T data set, a result attributed to NS&T sampling in areas of naturally (not contaminated) elevated Cr content. It remains undetermined, however, why the world-wide data set, even with exclusion of “hot spots”, yielded higher means and “highs” for Cd, Hg, As, and Ag. 相似文献
47.
Nada Horvatinčić José Luis Briansó Bogomil Obelić Jadranka Barešić Ines Krajcar Bronić 《Water, Air, & Soil Pollution: Focus》2006,6(5-6):475-485
The process of eutrophication in form of intense plant growth has been observed in some lakes and water streams at the Plitvice
Lakes National Park in central Croatia. Here we investigate whether this phenomenon is a consequence of anthropogenic pollution
or due to naturally produced organic matter in the lakes. We applied chemical analysis of water at two springs and four lakes
(nutrients, dissolved organic carbon (DOC), trace elements) and measurements of surface lake sediments (mineral and organic
fraction analyses, trace elements) in four different lakes/five sites. The chemical composition of water does not indicate
recent anthropogenic pollution of water because the concentrations of most trace elements are below detection limits. The
concentrations of DOC and nutrients are slightly higher in the area of increased eutrophication-plant growth. Also the content
of organic matter in the sediment is at the highest level in areas with highest C/N ratio indicating that the organic fraction of this sediment is mainly of terrestrial origin. There is no significant difference
among the trace element concentration in the upper segment of all cores, deposited approximately during last 50 years when
higher anthropogenic influence is expected due to development and touristic activity, and the lower part of the cores, corresponding
to the period approximately 100–200 years before present. The content of trace elements and organic matter in sediments decreases
from the uppermost lake downstream. According to our results there is no indication of recent anthropogenic pollution in water
and sediment. Higher concentrations of DOC in water as well as phosphorus and some other elements in the lake sediment can
be a consequence of input of natural organic matter to the lake water. 相似文献
48.
49.
详细研究了祁连—柴达木盆地北缘地区石炭系泥岩的微量元素和稀土元素地球化学特征。各微量元素在各剖面及不同层位变化相当复杂 ,但仍有一定规律 ,这种变化与其物源供应和沉积成岩环境有关。各样品稀土总量变化较大 ,以甘肃永昌煤山子剖面总量最高 ;各泥岩样品轻稀土富集 ,Eu负异常 ,δEu介于 0 .4 4~0 .90之间。微量、稀土元素组合及比值的变化 ,显示物源区母岩为花岗岩和玄武岩的混合 ,稀土分布模式显示源岩为粘土岩、花岗岩和中性岩的混合 ,两者示物源一致。元素的丰度及其比值 ,反映当时水介质环境大部分为海相 ,亦有部分为陆相 ,与其它相标志所表征的结果是一致的。 相似文献
50.