全文获取类型
收费全文 | 2522篇 |
免费 | 320篇 |
国内免费 | 913篇 |
专业分类
安全科学 | 273篇 |
废物处理 | 102篇 |
环保管理 | 191篇 |
综合类 | 1778篇 |
基础理论 | 381篇 |
污染及防治 | 549篇 |
评价与监测 | 177篇 |
社会与环境 | 204篇 |
灾害及防治 | 100篇 |
出版年
2024年 | 14篇 |
2023年 | 73篇 |
2022年 | 200篇 |
2021年 | 168篇 |
2020年 | 170篇 |
2019年 | 112篇 |
2018年 | 111篇 |
2017年 | 135篇 |
2016年 | 136篇 |
2015年 | 159篇 |
2014年 | 189篇 |
2013年 | 249篇 |
2012年 | 220篇 |
2011年 | 215篇 |
2010年 | 183篇 |
2009年 | 174篇 |
2008年 | 170篇 |
2007年 | 166篇 |
2006年 | 201篇 |
2005年 | 144篇 |
2004年 | 89篇 |
2003年 | 81篇 |
2002年 | 67篇 |
2001年 | 46篇 |
2000年 | 56篇 |
1999年 | 41篇 |
1998年 | 23篇 |
1997年 | 26篇 |
1996年 | 27篇 |
1995年 | 16篇 |
1994年 | 29篇 |
1993年 | 20篇 |
1992年 | 9篇 |
1991年 | 9篇 |
1990年 | 10篇 |
1989年 | 4篇 |
1988年 | 4篇 |
1987年 | 4篇 |
1986年 | 1篇 |
1985年 | 1篇 |
1982年 | 3篇 |
排序方式: 共有3755条查询结果,搜索用时 515 毫秒
111.
祁连山高山草甸土壤CO2通量的时空变化及其影响分析 总被引:1,自引:0,他引:1
采用Li-6400便携式光合作用测量系统连接Li-6400-09土壤呼吸室,在2004年生长季节对祁连山高山草甸土壤CO2通量沿海拔梯度进行了野外定位试验,统计分析了水热因子及根系生物量对高山草甸土壤CO2通量特征的可能影响.结果表明,土壤CO2通量存在明显的空间变化规律, 沿海拔梯度土壤CO2通量随着海拔梯度的增加而逐渐减小,其变异系数逐渐增加;就日变化而言,土壤CO2通量晚间维持在较低水平,02:00~06:00最低,在07:00~08:30开始升高,11:00~16:00达到峰值,16:00~18:30开始下降,整个过程呈单峰曲线.土壤CO2通量的日平均值介于(0.56±0.32) ~ (2.53±0.76) μmol·(m2·s)-1.从季节变化来看,土壤CO2通量均以夏秋季较高,春冬季排放量较低,7~8月份达到最大值[4.736 μmol·(m2·s)-1],6月与9月份次之,5月与10月份基本一致,整个生长过程总的变化趋势呈单峰曲线形式.高山草甸土壤CO2通量在植物生长季与10 cm土壤温度、土壤含水量、根系生物量都存在不同程度的正相关关系,表明高山草甸土壤CO2通量的空间变异主要受温度、水分和植物根系的综合影响. 相似文献
112.
113.
Assessing field vulnerability to phosphorus loss in Beijing agricultural area
using Revised Field Phosphorus Ranking Scheme 总被引:1,自引:0,他引:1
Guanting Reservoir,one of the drinking water supply sources of Beijing,suffers from water eutrophication.It is mainly supplied by Guishui River.Thus,to investigate the reasons of phosphorus(P)loss and improve the P management strategies in Guishui River watershed are important for the safety of drinking water in this region.In this study,a Revised Field P Ranking Scheme(PRS)was developed to reflect the field vulnerability of P loss at the field scale based on the Field PRS.In this new scheme,six factors are included, and each one was assigned a relative weight and a determination method.The affecting factors were classified into transport factors and source factors,and,the standards of environmental quality on surface water and soil erosion classification and degradation of the China were used in this scheme.By the new scheme,thirty-four fields in the Guishui River were categorized as"low","medium"or"high"potential for P loss into the runoff.The results showed that the P loss risks of orchard and vegetable fields were higher than that of corn and soybean fields.The source factors were the main factors to affect P loss from the study area.In the study area,controlling P input and improving P usage efficiency are critical to decrease P loss.Based on the results,it was suggested that more attention should be paid on the fields of vegetable and orchard since they have extremely high usage rate of P and high soil test of E Compared with P surplus by field measurements,the Revised Field PRS was more suitable for reflecting the characteristics of fields,and had higher potential capacity to identify critical source areas of P loss than PRS. 相似文献
114.
115.
海河沉积物对菲的吸附解吸行为研究 总被引:2,自引:0,他引:2
采用北运河坝河断面、海河干流邓善沽断面及葛沽镇断面表层沉积物及南开花园土为吸附剂,以菲为吸附质进行一系列吸附动力学和吸附-解吸平衡实验研究。结果表明,菲在各颗粒物上的吸附动力学过程,在0-4h内基本可达吸附平衡,刚开始吸附速率很快,然后迅速降低,并逐渐稳定;菲在各颗粒物上的等温平衡吸附可用线性等温线方程及Freundlich方程较好的拟合;不同来源颗粒物对菲的吸附能力随颗粒物中有机质含量增加而增强;葛沽镇颗粒物经高温灼烧处理后,其吸附能力明显降低;各天然颗粒物及不同温度灼烧处理的颗粒物对菲的解吸行为存在不同程度的滞后,灼烧颗粒物的滞后性远远大于原颗粒物,颗粒物中的有机质组分及性质对菲的解吸滞后有重要影响 相似文献
116.
117.
为了促进西北干旱区中小城市的快速、稳定的发展,解决该地区中小城市的水资源短缺问题,以水价作为出发点,充分利用水价格的经济杠杆作用,制定出该地区中小城市的水价。以西北干旱区中具有代表性的城市石河子为例,通过实地调研,得到石河子居民、居民生活用水情况、现行水价、居民家庭节水情况、居民的心理承受水价以及平时生活的节水意识等情况,通过分析,得出居民的心理承受偏低,现行水价仍有一定的上调空间,调价范围为1.58~2.31元/m3,最高可调至4.11元/m3。结合石河子的水价,为西北干旱区的中小城镇的水价改革、提高水资源的利用率等提出一些切实可行的建议。 相似文献
118.
Biosorption of silver ions onto Bacillus cereus biomass was investigated. Overall kinetic experiments were performed for the
determination of the necessary contact time for the attainment of equilibrium. It was found that the overall biosorption process was
best described by pseudo second-order kinetic model. The crystals detected by scanning electron microscope and X-ray photoelectron
spectroscopy suggested the precipitation was a possible mechanism of biosorption. The molecular genetics of silver resistance of B.
cereus biomass was also detected and illustrated by a whole cell sensor tool. 相似文献
119.
Application of Ruditapes Philippinarum conglutination mud (RPM) for decolorizing synthetic dye solutions was studied. RPM showed good activity for decolorization of Methylene Blue, Crystal Violet, Malachite Green, and Ink Blue. The amount of the RPM had great effect on the decoloration rate of the dye solutions. However, the decoloration rate did not continue to increase when the amount of mud exceeded the optimum dose. The temperature of the dye solution had a remarkable effect on the decolorization rate of Ink Blue solution, but had little effect on the other three dye solutions. The initial pH of the dye solutions evidently affected the decolorization rate of Malachite Green solution, but had less effect on the other three. The decolorization rate of the dye solutions increased significantly with treatment time within 8 hr, but tended to be steady after 8 hr for Methylene Blue, Crystal Violet and Malachite Green solutions, and after 12 hr for Ink Blue solution. The decolorization efficiencies for the four dye solutions under the optimum conditions were all above 90%. Seventeen strains screened from RPM showed flocculation ability for kaolin clay suspension. Out of them, the flocculation rate of strain ZHT3-9 and strain ZHT4-13 were up to 88.14% and 86.01%, respectively. ZHT3-9 was studied, and its decolorization rate for Methylene Blue, Crystal Violet, and Malachite Green reached 90.02%, 89.21%, and 80.29%, respectively. By morphological, physiological and biochemical characteristics analysis and 16S rRNA sequencing, the strain ZHT3-9 was identified as Arthrobacter sp. 相似文献
120.
针对钱塘江杭州段水污染现状,对钱塘江杭州段12个采样断面的沉积物进行了系统研究。结果表明,沉积物Fe、Mn的平均含量分别为2.05%,449 mg/kg,变异系数分别为16%、27%。主成分分析结果表明,Fe、Mn、K具有一定的同源性,代表沉积物的自然来源,Fe、Al的分布情况反映两者之间可能存在一定的同源性。相关性分析结果表明,Fe、Al、K均与粘粒显著或极显著相关,反映了地球化学作用和水文条件相互作用的结果;Mn与有机污染(OM)呈显著负相关,说明Mn的污染源与OM不存在同源性,相反,有机质污染导致沉积物锰含量有所降低,两者可能存在密切关系。 相似文献