全文获取类型
收费全文 | 551篇 |
免费 | 63篇 |
国内免费 | 395篇 |
专业分类
安全科学 | 19篇 |
废物处理 | 8篇 |
环保管理 | 36篇 |
综合类 | 521篇 |
基础理论 | 322篇 |
污染及防治 | 49篇 |
评价与监测 | 8篇 |
社会与环境 | 28篇 |
灾害及防治 | 18篇 |
出版年
2024年 | 2篇 |
2023年 | 15篇 |
2022年 | 29篇 |
2021年 | 49篇 |
2020年 | 32篇 |
2019年 | 28篇 |
2018年 | 36篇 |
2017年 | 49篇 |
2016年 | 38篇 |
2015年 | 50篇 |
2014年 | 46篇 |
2013年 | 73篇 |
2012年 | 54篇 |
2011年 | 50篇 |
2010年 | 39篇 |
2009年 | 46篇 |
2008年 | 25篇 |
2007年 | 40篇 |
2006年 | 39篇 |
2005年 | 39篇 |
2004年 | 25篇 |
2003年 | 25篇 |
2002年 | 24篇 |
2001年 | 19篇 |
2000年 | 24篇 |
1999年 | 17篇 |
1998年 | 11篇 |
1997年 | 12篇 |
1996年 | 11篇 |
1995年 | 10篇 |
1994年 | 10篇 |
1993年 | 20篇 |
1992年 | 8篇 |
1991年 | 3篇 |
1990年 | 5篇 |
1989年 | 3篇 |
1988年 | 2篇 |
1987年 | 1篇 |
排序方式: 共有1009条查询结果,搜索用时 46 毫秒
41.
Runoff and sediment losses from 27 upland catchments in Southeast Asia: Impact of rapid land use changes and conservation practices 总被引:5,自引:0,他引:5
C. Valentin F. Agus R. Alamban A. Boosaner J.P. Bricquet V. Chaplot T. de Guzman A. de Rouw J.L. Janeau D. Orange K. Phachomphonh Do Duy Phai P. Podwojewski O. Ribolzi N. Silvera K. Subagyono J.P. Thibaux Tran Duc Toan T. Vadari 《Agriculture, ecosystems & environment》2008,128(4):225-238
Rapid changes in upland farming systems in Southeast Asia generated predominantly by increased population pressure and ‘market forces’ have resulted in widespread land degradation that has been well documented at the plot scale. Yet, the links between agricultural activities in the uplands and downstream off-site effects remain largely unknown because of the difficulties in transferring results from plots to a larger scale. Many authors have thus pointed out the need for long-term catchment studies. The objective of this paper is to summarize the results obtained by the Management of Soil Erosion Consortium (MSEC) over the last 5 years from 27 catchments in five countries (Indonesia, Laos, Philippines, Thailand, and Vietnam). The purpose of the study was to assess the impacts of cultivation practices on annual runoff and erosion rates. Initial surveys in each catchment included topography, soils and land use. Monitoring included climatic, hydrologic and erosion (total sediment yield including bed load and suspended sediment load) data, land use and crop yields, and farmers’ income. In addition, new land management options were introduced through consultations with farmers and evaluated in terms of runoff and erosion. These included tree plantations, fruit trees, improved fallow with legumes, maize intercropped with legumes, planted fodder, native grass strips and agro-ecological practices (direct sowing and mulch-based conservation agriculture). Regressions analyses showed that runoff during the rainy season, and normalized runoff flow coefficient based on erosive rainfall during the rainy season (rainfall with intensity exceeding 25 mm h−1) increase with the percentage of the catchment covered by maize. Both variables decrease with increasing soil depth, standard deviation of catchment slope (that reflects terrain roughness), and the percentages of the catchment covered by fallow (regular and improved), tree plantations and planted fodder. The best predictors of sediment yield were the surface percentages of maize, Job's tears, cassava and footpaths. The main conclusions generated from this study were: (i) soil erosion is predominantly influenced by land use rather than environmental characteristics not only at the plot scale but also at the catchment scale; (ii) slash-and-burn shifting cultivation with sufficiently long rotations (1 year of cultivation, 8 years of fallow) is too often unjustly blamed for degradation; (iii) in its place, continuous cropping of maize and cassava promotes high rates of soil erosion at the catchment scale; (iv) conservation technologies are efficient in reducing runoff and total sediment yield at the catchment scale; (v) the adoption of improved soil management technologies by upland farmers is not a function of the degree of intensification of their farming system and/or of their incomes. The results suggest that if expansion of maize and cassava into already degraded upland systems were to occur due to increased demand for biofuels, there is a risk of higher runoff and sediment generation. A failure to adopt appropriate land use management strategies will result in further rapid resource degradation with negative impacts to downstream communities. 相似文献
42.
来源于土壤和灌溉水的砷在水稻根表及其体内的富集特性 总被引:6,自引:2,他引:4
采用土壤-玻璃珠联合培养的方式,选择2个氧化能力不同的水稻品种YY-1、94D-64(品系)和采自浙江富阳的土壤(砷的本底值为13.8 mg·kg-1),并设灌溉清水和含砷水2个处理(即在分蘖期、拔节期、孕穗期、开花期和灌浆期5个生育阶段灌溉含砷污水,随灌溉水进入土壤中砷的浓度为3.2mg·kg-1),研究了砷在土壤-根表铁氧化物-水稻系统中的累积规律以及土壤和灌溉水对水稻秸秆和籽粒富集砷的贡献程度.结果表明,水稻的秸秆生物量及其籽粒产量并没有受到不同来源砷的显著影响;灌溉含砷水处理的两品系水稻根表铁氧化物沉积的数量(YY-1∶196 g·kg-1,94D-64∶75.8 g·kg-1)高于对照(YY-1∶175g·kg-1,94D-64∶60.1 g·kg-1),但差异不显著.然而,在水稻5个不同的生育期灌溉含砷水均显著增加了砷在其根表及其体内不同部位的富集(94D-64籽粒中砷含量除外).没有灌溉含砷水的对照其秸秆和籽粒中累积的砷来源于土壤,而砷处理的水稻其秸秆和籽粒中富集的砷则来源于土壤和灌溉的含砷水.土壤对YY-1和94D-64秸秆中富集砷的贡献率分别为76.5%和71.O%,灌溉水的贡献率分别为23.5%和29.0%,2个水稻品系之间没有明显差异.YY-1籽粒中的砷66.4%来源于土壤,33.6%来源于含砷灌溉水,灌溉水对该品系籽粒中砷的富集贡献率较高.另一品系94D-64籽粒中砷84.8%来源于土壤,15.2%由灌溉水贡献,灌溉水对此品系籽粒累积砷的贡献率较低.来源于土壤和灌溉水的砷在水稻籽粒中的富集没有超出我国的国家食品卫生标准(0.7 mg·kg-1). 相似文献
43.
44.
以稻草和污泥为碳源硫酸盐还原菌处理酸性矿山排水 总被引:9,自引:4,他引:5
以污泥为硫酸盐还原菌(SRB)接种菌群,分别添加等量稻草和乙醇,研究了SRB以不同碳源处理酸性矿山排水(pH=2.5)的过程及不同碳源对硫酸盐还原和重金属去除的影响.结果表明,在无外加中和剂的情况下,污泥中的碱性物质可在反应开始的1 d内迅速中和酸性矿山排水的部分酸度,使反应体系pH值从2.5升至5.4~6.3,利于SRB的生长.污泥中含少量易被微生物分解的有机物,体系中仅含污泥时,SO24-还原率最低(65.9%).添加稻草可促进SO24-还原(79.2%),因为污泥中的水解菌加速稻草分解,为SRB提供相对充足的碳源.添加乙醇为对照试验的体系中SO24-还原率最高(97.9%).含污泥的反应体系Cu2+去除率均高于99%,SRB驯化前Cu2+的去除主要归因于污泥的吸附作用.以稻草和污泥为碳源可实现低成本酸性矿山排水处理,对矿山环境的原位修复有实际意义. 相似文献
45.
46.
47.
Jinfei Feng Yinxi Wang Jian Zhao Liqun Zhu Xinmin Bian Weijian Zhang 《环境科学学报(英文版)》2011,23(7):1158-1164
Air and soil pollution from traffic has been considered as a critical issue to crop production and food safety, however, few efforts have
been paid on distinguish the source origin of traffic-related contaminants in rice plant along highway. Therefore, we investigated metals
(Pb, Cd, Cr, Zn and Cu) concentrations and stable Pb isotope ratios in rice plants exposed and unexposed to highway traffic pollution
in Eastern China in 2008. Significant differences in metals concentrations between the exposed and unexposed plants existed in leaf for
Pb, Cd and Zn, in stem only for Zn, and in grain for Pb and Cd. About 46% of Pb and 41% of Cd in the grain were attributed to the
foliar uptake from atmosphere, and there were no obvious contribution of atmosphere to the accumulations of Cr, Zn and Cu in grain.
Except for Zn, all of the heavy metals in stem were attributed to the root uptake from soil, although significant accumulations of Pb and
Cd from atmosphere existed in leaf. This indicated that different processes existed in the subsequent translocation of foliar-absorbed
heavy metals between rice organs. The distinct separation of stable Pb isotope ratios among rice grain, leaf, stem, soil and vehicle
exhaust further provided evidences on the different pathways of heavy metal accumulation in rice plant. These results suggested that
further more attentions should be paid to the atmospheric deposition of heavy metals from traffic emission when plan crop layout for
food safety along highway. 相似文献
48.
通过研究广东省江门市三个不同优质稻产地土壤中相同元素对水稻品质造成不同影响的特点,如都斛土壤中的N与水稻胶稠度呈正相关关系,而在牛江则呈较强负相关关系;都斛土壤中的Mo与水稻的不完善粒呈较强负相关关系,而在牛江则呈正相关关系。根据吸收系数与土壤营养元素关系,得出作物对营养元素的吸收限。当土壤能给作物提供足够的营养元素时,作物对土壤营养元素的吸收存在一个极限,土壤元素含量接近这个极限时,作物对元素的吸收达到饱和,对元素的吸收系数则低;当土壤营养元素供给能力不足时,作物对营养元素吸收能力较强,对元素吸收系数较高。通过对比各元素及指标与稻谷感官品质相关关系并评分,得出土壤营养元素含量越偏离水稻对营养元素的吸收限,则对水稻品质的影响越大的结论,由此解释了不同省份农业地质调查中农作物元素与土壤元素相关关系混乱甚至矛盾的问题,为水稻的施肥提供了科学合理的依据 相似文献
49.
50.
氮肥水平对不同土壤CH4排放的影响 总被引:10,自引:3,他引:7
鉴于氮肥施用对农田CH4排放的影响还有很大不确定性,室外盆栽试验于2002年在南京农业大学实施.选取3个供试土壤,各土壤设置对照和低、中、高3个不同氮肥水平,施入尿素量分别为0 g/盆钵(对照) ,0.64g/盆钵,(低氮水平) ,1.28g/盆钵(中氮水平) ,1.93g/盆钵(高氮水平) .结果表明在水稻生长季,不同氮肥(尿素)施用量对稻田土壤CH4排放影响表现为不同土壤之间,及不同氮肥水平之间CH4排放均存在显著差异.无氮肥施入的情况下,3种土壤的CH4季节性累积排放量存在显著差异,分别为6.7g/m2,12.6g/m2 和8.3g/m2.施加氮肥后,3种土壤的CH4排放量随氮肥施入量的增加,均表现为降低趋势,不同土壤CH4排放量存在差异,土壤背景氮含量最高的F(江苏溧水)土壤的CH4排放都比相应氮肥水平下的G(江苏涟水)和H(江苏农科院)土壤的CH4排放低1倍左右.更进一步发现从低氮到中氮水平,3种土壤CH4排放量随氮肥用量的增加降低幅度最大,而此时各土壤的NH4-N含量随氮肥用量增加明显提高,推断造成CH4排放降低的主要可能原因是各土壤的氨态氮含量的增加所致.从中氮到高氮水平3种土壤的CH4排放量的变化不尽相同,G和H土壤的CH4排放量随氮肥用量的增加而降低,而F土壤在中氮和高氮水平下的CH4排放量没有明显变化,值分别为30g/m2. 相似文献