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831.
提出了将Sobel边缘检测算子与深度卷积神经网络(CNN)算法结合的方法(E-ConvNet),用于污染场地的ERT反演过程.通过Sobel算子提取污染区域视电阻率数据的边缘特征作为CNN的先验信息,提高E-ConvNet的计算效率及识别精度.在5种理论模型(单异常体、双异常体及含双异常体的层状结构)和现场实例上测试了E-ConvNet算法的性能,并与最小二乘算法(LS)比较.测试结果表明:E-ConvNet能够准确识别污染处的面积、位置及阻值,其识别精度和计算效率均优于LS.E-ConvNet的单异常识别准确率为81.8%~84.9%,而LS则仅为9.6%~36.2%;多异常识别准确率为68.6%~84.4%,LS仅为2.8%~27.6%;E-ConvNet用时约为112~190ms,LS耗时为6000~7000ms.因此,在污染场地调查工作中,E-ConvNet能够准确高效地反演出污染区域的位置及范围,为开展后续评估/修复工作提供技术支持.  相似文献   
832.
Forestry Best Management Practices (BMPs) were developed to protect water quality. In the eastern US, those BMPs were often expanded to include maintenance of site productivity. Generally, BMPs recommend the use of pre-harvest planning and careful design for construction of roads and other activities that expose bare soil, minimizing trafficking and areas of bare soil, maintaining streamside management zones, ensuring rapid revegetation following harvesting, minimizing soil disturbance, and ameliorating severe trafficking with site preparation. This review of peer-reviewed research from the past 20 years examined the effects of forest harvesting and site preparation on water quality and site productivity in the eastern US. The review was subdivided into areas having relatively similar physiography and land management (New England, Lake States, Appalachian Plateau, Ridge and Valley, Blue Ridge, Piedmont, Atlantic Coastal Plain, Gulf Coastal Plain, and Ouachitas-Ozarks). In general, data from steeper physiographic regions indicated that forest harvesting and site preparation can increase erosion, sediment and nutrient losses to streams. However, the quantities introduced into streams tended to be relatively low, generally below the values that are considered acceptable for alternative land uses. Also most research indicated that water quality recovers within two to five years following forest operation disturbances, particularly if BMPs are employed. Research from the less mountainous and often more poorly drained Lake States and Coastal Plain regions indicated that soil compaction and rutting may or may not cause site productivity effects, depending on soil types, natural ameliorative properties and site preparation. Overall, the research supports the forestry BMPs recommended in the eastern states.  相似文献   
833.
Replicate intact peat/vegetation monoliths were collected along a pollution gradient in the UK and subjected over one year to 1200 mm of simulated rainfall of the same chemical composition as they received in the field. Drainage water was analysed periodically for DOC and pH, and the decomposition rates of Calluna vulgaris and Eriophorum angustifolium leaves were measured, as well as soil atmosphere CO2 contents and peat matric potentials. the chemical characteristics of the peats as initially sampled from the field also were determined. the results suggest that acidic precipitation has induced chemical changes in ombrotrophic peats, lowering their pH and base status, when due account is taken of calcium deposition or any mineral content. Greater DOC fluxes were observed from the more acid peats, and litter decomposition rates from these peats were reduced.  相似文献   
834.
The results of an experimental study on the behaviour of 134Cs, 85Sr and 65Zn in processing tomato plants grown in peat substrate are presented. Plants were contaminated by wet deposition of 134Cs, 85Sr and 65Zn, either by sprinkling the above ground part at two phenological stages or by administering 134Cs, 85Sr and 65Zn to the soil. The plants contaminated at the second phenological stage intercepted 38.3% less than those contaminated at the first stage, although leaf area increased by more than double. Transfer coefficients from peat soil to ripe fruit for 134Cs are significantly higher than those for 85Sr and 65Zn. Leaf to fruit transfer coefficients for 134Cs are one order of magnitude higher than for 65Zn and two orders higher than for 85Sr. Only when deposition affects fruits, as at the second phenological stage, are transfer coefficients to fruits similar for the three radionuclides.  相似文献   
835.
A Chronology of Nitrogen Deposition in the UK Between 1900 and 2000   总被引:2,自引:0,他引:2  
Measurements of the concentrations of nitrogen compounds in air and precipitation in the UK have been made since the mid-19th century, but no networks operating to common protocols and having traceable analytical procedures were established until the 1950s. From 1986 onwards, a high-quality network of sampling stations for precipitation chemistry was established across the UK. In the following decade, monitoring networks provided measurement of NO2, NH3, HNO3 and a satisfactory understanding of the dry deposition process for these gases allowed dry deposition to be quantified. Maps of N deposition for oxidized and reduced compounds at a spatial scale of 5 km × 5 km are available from 1986 to 2000. Between 1950 and 1985, the more limited measurements, beginning with those of the European Air Chemistry Network (EACN) provide a reasonable basis to estimate wet deposition of NO 3 –N and NH 4 + –N. For the first half of the century, estimates of deposition were scaled with emissions assuming a constant relationship between emission and deposition for each of the components of the wet and dry deposition budget at the country scale. Emissions of oxidized N, which dominated total nitrogen emissions throughout the century, increased from 312 kt N annually in 1900 to a peak of 787 kt for the decade 1980–1990 and then declined to 460 kt in 2000. Emissions of reduced N, largely from coal combustion were about 168 kt N in 1900, increasing to a peak of 263 kt N in 2000 and by now dominated by agricultural sources. Reduced N dominated the deposition budget at the country scale, increasing from 163 kt N in 1900 to 211 kt N in 2000, while deposition of oxidized N was 66 kt N in 1900 and 191 kt N in 2000. Over the century, 68 Mt (Tg) of fixed N was emitted within the UK, 78% as NO x , while 29 Mt of nitrogen was deposited (43% of emissions), equivalent to 1.2 t N ha–1, on average, with 60% in the reduced form. Deposition to semi-natural ecosystems is approximately 15 Tg N, equivalent to between 1 and 5 t N ha–1, over the century and appears to be accumulating in soil. The N deposition over the century is similar in magnitude to the total soil N inventory in surface horizons.  相似文献   
836.
本研究以某典型焦化厂建构筑物及生产设施为对象,从不同功能区、不同材质等角度分析建构筑物及生产设施表面多环芳烃(PAHs)的赋存特征,并评价其健康风险.结果表明,焦化厂建构筑物及生产设施表面的PAHs含量范围为8. 00×10~(-2)~1. 98×102μg·dm~(-2).其中,22. 0%的擦拭样品PAHs含量超出了世界贸易中心工作组(WTCTG)的规定限值(1. 45μg·dm~(-2)),PAHs最大超标可达135倍.PAHs含量高值主要分布在炼焦区和精制区,其中,炼焦区样品PAHs含量均值最高,达12. 1μg·dm~(-2).研究区中防锈漆材质表面PAHs含量均值和超标率最高,砖和水泥次之,玻璃对PAHs的吸附和富集能力最小.采用美国超级基金方法对各功能区开展健康风险评估研究,其中,炼焦区及精制区内PAHs存在致癌风险,其致癌单体对暴露人群的总致癌风险值可达3. 78×10~(-6)~1. 32×10~(-5),均高于US EPA标准下限10~(-6).场地建构筑物及生产设施表面的有机污染物分布规律及健康风险结果可为污染场地环境管理和治理对策提供科学依据.  相似文献   
837.
人类活动背景下,氮(N)沉降持续影响着生态系统的碳循环.氮沉降对土壤有机碳的影响与不同碳组分的差异性响应有关.为探究短期氮沉降背景下土壤有机碳组分变化及其影响因素,基于野外氮添加试验,以刺槐人工林为研究对象,共设置4个氮添加梯度:0(CK)、1.5(N1)、3(N2)和6(N3) g·(m2·a)-1,分别在6月和9月进行取样,测定土壤理化性质、微生物生物量和酶活性.结果表明:(1)外源氮输入降低了土壤pH,促进可溶性有机碳含量的增加,增加了土壤氮素有效性.(2)短期氮添加显著降低了土壤有机碳含量,且有机碳各组分对氮添加响应不同.其中,易氧化有机碳含量显著降低,且在N2处理下达到最低,与对照相比分别降低了54.4%和48.2%,惰性有机碳含量增加,但增加不显著.氮添加降低了土壤碳库活度,提高了土壤碳库的稳定性.土壤碳库活度分别在N3和N2处理下达到最低,与对照相比分别降低了53.3%和52.80%.(3)随机森林模型表明,短期氮添加下土壤微生物生物量化学计量比、微生物生物量碳和AP是驱动土壤有机碳活度变化的关键因子,分别解释了易氧化有机碳和惰...  相似文献   
838.
河流水体和沉积物中酚类EDCs因其广泛存在和危害持久受到广泛关注,为研究自然条件下河流沉积物上多种酚类EDCs共存的吸附行为,本文以苯酚(phenol)和双酚A(bisphenol A,BPA)为目标污染物,灞河表层沉积物为吸附剂,通过静态吸附实验研究二者在单溶质和双溶质体系下的吸附等温特性,在此基础上,采用位点能量分布理论分析污染物之间的竞争吸附机理.结果表明,相同浓度(1~50 mg·L~(-1))条件下,单溶质体系的苯酚吸附位点主要集中于高能量位;双酚A吸附位点主要分布于低能量区.双溶质体系下,相同浓度的两种物质位点分布函数均随着位点能量的增大而呈指数降低,苯酚下降趋势较为平缓,吸附位点分布更均匀.两种体系相比较,双溶质体系下苯酚平均位点能量和位点能量非均质性分别降低0.867%和3.473%,吸附位点数量降低1.230%;双酚A平均位点能量和位点能量非均质分别增大了6.074%和14.992%,吸附位点数量增大6.389%.即双溶质体系下,二者之间存在一定的竞争吸附,双酚A处于竞争优势.  相似文献   
839.
渤海湾大气金属元素沉降和来源解析研究   总被引:3,自引:0,他引:3  
干湿沉降是污染物从大气进入到地表生态环境的主要途径.渤海湾临近大气污染严重的京津冀地区,同时受航运交通排放影响,但渤海湾大气金属元素沉降量及其来源并不十分清楚.本研究于2016年11月—2017年10月在渤海西岸采集了大气沉降样品,利用电感耦合等离子体质谱仪(ICP-MS)对样品中25种金属元素的含量进行了测定分析,估算了大气金属沉降量并进行了源解析.结果表明:沉降样品中25种元素的浓度变化范围为2458.8μg·L~(-1)(Ca)~9.9 ng·L~(-1)(Th),年沉降量变化为1229.9 mg·m~(-2)·a~(-1)(Ca)~5.0μg·m~(-2)·a~(-1)(Th).受降水量季节分布的影响,多数金属元素的沉降量在夏季最高,春秋季较低.除Be、Fe、Ni、Cr、Al、Th和U等元素外,其余18种元素都有不同程度的富集,特别是Cd、Ag、Se和Sb等元素已高度富集.燃煤(12.8%)、扬尘(25.9%)、工业(33.1%)和航运(28.2%)是渤海湾沉降样品中金属元素的主要来源,尤其是航运排放对海湾大气Sb、Cd和Mo沉降具有显著贡献.研究结果可为京津冀区域海陆协同发展和环境质量改善提供科学参考.  相似文献   
840.
以京蒙沙源区大河口水库为研究对象,于2017年1月~12月对水库周围布设的12个大气沉降监测站点收集样品144个,测定大气干、湿沉降物中TN浓度,计算大气总氮干、湿沉降通量,分析大气TN干、湿沉降污染特征及季节性变化特征.另选取水库周边不同典型地块,布设14个采样点采集样品76个,测定土壤δ15N-TN含量水平,解析水库大气氮沉降主要来源,并借助HYSPLIT4气团后向轨迹模型分析各季节不同类型气团输移营养盐对大河口水库的影响.结果表明:水库全年大气TN干沉降通量变化范围为122.44~425.64kg/(km2·month),平均值为200.83kg/(km2·month);湿沉降通量变化范围1.23~188.89kg/(km2·month),平均值为66.33kg/(km2·month).大气总氮年沉降通量为3205.9kg/(km2·a),约为全国氮沉降平均水平(790kg/(km2·a))的4.06倍.从沉降类型上来看,大气沉降主要以干沉降为主,占沉降总量的75.17%,湿沉降占总沉降通量的24.83%.大气氮干沉降通量表现为春、秋季节明显高于夏、冬季节,湿沉降通量春、夏季明显高于秋、冬季节的季节性变化规律.通过对典型地块δ15N-TN同位素数据分析,表明夏季有71.4%的大气沉降样品来源于不可分辨的混合源输入,春、秋、冬季大河口水库超过45%的样品来源于沙地,另一大污染源为研究区周围的耕地.运用HYSPLIT4后向轨迹模型证明,从蒙古国入境的气团对研究区污染物大气输移影响较大,冬季采暖期间的大气污染和春季频繁发生的沙尘暴是造成北方沙区水体春季水环境变差的因素之一.  相似文献   
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