全文获取类型
收费全文 | 20951篇 |
免费 | 5863篇 |
国内免费 | 28292篇 |
专业分类
安全科学 | 2972篇 |
废物处理 | 535篇 |
环保管理 | 1885篇 |
综合类 | 35844篇 |
基础理论 | 3979篇 |
污染及防治 | 6162篇 |
评价与监测 | 1963篇 |
社会与环境 | 896篇 |
灾害及防治 | 870篇 |
出版年
2024年 | 156篇 |
2023年 | 453篇 |
2022年 | 986篇 |
2021年 | 973篇 |
2020年 | 1666篇 |
2019年 | 2288篇 |
2018年 | 2437篇 |
2017年 | 2586篇 |
2016年 | 2258篇 |
2015年 | 2749篇 |
2014年 | 3346篇 |
2013年 | 3663篇 |
2012年 | 3835篇 |
2011年 | 3422篇 |
2010年 | 3103篇 |
2009年 | 3050篇 |
2008年 | 2593篇 |
2007年 | 2617篇 |
2006年 | 2054篇 |
2005年 | 1569篇 |
2004年 | 1318篇 |
2003年 | 998篇 |
2002年 | 816篇 |
2001年 | 813篇 |
2000年 | 882篇 |
1999年 | 696篇 |
1998年 | 463篇 |
1997年 | 441篇 |
1996年 | 470篇 |
1995年 | 422篇 |
1994年 | 273篇 |
1993年 | 205篇 |
1992年 | 281篇 |
1991年 | 262篇 |
1990年 | 227篇 |
1989年 | 197篇 |
1988年 | 145篇 |
1987年 | 72篇 |
1986年 | 74篇 |
1985年 | 53篇 |
1984年 | 58篇 |
1983年 | 40篇 |
1982年 | 45篇 |
1981年 | 34篇 |
1980年 | 1篇 |
1979年 | 2篇 |
1978年 | 3篇 |
1976年 | 1篇 |
1972年 | 5篇 |
1971年 | 5篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
71.
72.
Geng Jinju Wang Qiang Niu Xiaojun Wang Xiaorong 《Frontiers of Environmental Science & Engineering in China》2007,1(1):120-124
Effects of pH, temperature, and oxygen on the production and release of phosphine in eutrophic lake sediments were investigated
under laboratory tests. Results indicated that the elimination of matrix-bound phosphine was accelerated under initial pH
1 or 12. Phosphine levels could reach maximum under initial pH 10. The contents of phosphine increased with the addition of
alkali under pH 4–12. The rates of phosphine production and release from lake sediments varied with temperature. 20°C was
the most favorable temperature for the production of matrix-bound phosphine. Oxygen showed little effect on matrix-bound phosphine.
Matrix-bound phosphine concentrations in lake sediments were concluded to be dependent on a balance of natural generation
and depletion processes.
Translated from Acta Scientise Circumstantiae, 2005, 25(5): 681–685 [译自: 环境科学学报] 相似文献
73.
In this study, the two-stage upflow anaerobic sludge blanket (UASB) system and batch experiments were employed to evaluate
the performance of anaerobic digestion for the treatment of high concentration methanol wastewater. The acid resistance of
granular sludge and methanogenic bacteria and their metabolizing activity were investigated. The results show that the pH
of the first UASB changed from 4.9 to 5.8 and 5.5 to 6.2 for the second reactor. Apparently, these were not the advisable
pH levels that common methanogenic bacteria could accept. The methanogenic bacteria of the system, viz. Methanosarcina barkeri,
had some acid resistance and could still degrade methanol at pH 5.0. If the methanogenic bacteria were trained further, their
acid resistance would be improved somewhat. Granular sludge of the system could protect the methanogenic bacteria within its
body against the impact of the acidic environment and make them degrade methanol at pH 4.5. The performance of granular sludge
was attributed to its structure, bacteria species, and the distribution of bacterium inside the granule.
Translated from Acta Scientiae Circumstantiae, 2004, 24(4): 633–636 [译自: 环境科学学报] 相似文献
74.
对滇池湖滨区农村环境现状及主要环境问题进行了详细分析,就工程总体思路、设计原则及主要考核指标体系等进行了探讨,提出沿湖农村非点源污染防治工程技术方案,即通过以沼气池为纽带的农村能源结构改造、村级污水处置处理和配套沟渠系统建设、村内垃圾处理处置以及普及卫生旱厕、村庄道路修缮及绿化等工程和管理措施,从源头上控制污染物产生量,减少入湖污染负荷,有效地解决滇池环湖新农村建设中的环境保护问题。 相似文献
75.
76.
77.
沼泽红假单胞菌H3对酸性红B2GL染料的厌氧脱色和降解作用 总被引:7,自引:0,他引:7
从印染厂污泥中分离到一株沼泽红假单胞菌(RhodopseudomonaspalustrisH3),在光照厌氧条件下该菌生长细胞可将100mg/L酸性红B2GL染料去除到30mg/L.完整细胞脱色的最适条件为pH70,温度30℃,细胞浓度20—25mg/mL(湿重).低浓度的阳离子对脱色影响不大.在通Ar气使严格厌氧和加有还原性辅酶I的条件下无细胞提取液的脱色活性最高,比活率为154×10-2mg/(mg·h).根据降解产物的分析,推断了该菌对酸性红染料的降解代谢途径. 相似文献
78.
Stratigraphy, lithology and depositional structures of Liassic red limestone-breccias of the Adnet Formation, including the 'Adnet Scheck', were studied at several outcrops of the Northern Calcareous Alps (NCA) south-east of Salzburg. A four-fold lithostratigraphic division is proposed for the Adnet Formation of the Osterhorn Mountains: the hemipelagic Schmiedwirt (Sinemurian) and Kehlbach (Carixian) members are separated from the pelagic Saubach Member (Toarcian) by a layer of amalgamated breccias (Scheck Member, probably Domerian to early Toarcian). Several other breccia beds occur locally from the base of the Kehlbach Member up to the lower Saubach Member. Although the sediments overlying the Scheck Member breccias are of coeval age, the ages of the underlying strata are very different. This can be explained by submarine Liassic erosion during a period of resedimentation from the middle Carixian until the early Toarcian. At least 10–15?m of partly lithified sediments were eroded by gravity flows. The entire Kehlbach Member and up to two-thirds of the Schmiedwirt Member were removed at Adnet. The breccias originated from submarine debris flows. Repeated flows over a long period and the depositional setting exclude a triggering by sea-level fluctuations. Most probably they arose from tectonically triggered slumps and slides of superficial sediments. The 'Scheck' was initiated on the steep upper slope of the drowned Triassic Adnet reef and flowed to the north-east.The Pliensbachian to early Toarcian period of tectonic activity indicated by the breccias was the most important during the Liassic in the Osterhorn Mountains and other parts of the NCA. From the large-scale regional distribution of the breccias and in accord with published data, a roughly north-east trending strike-slip fault zone is proposed, crossing the NCA south of the Osterhorn block, with a peaking activity during the Pliensbachian to early Toarcian as the cause of the tectonic movements. 相似文献
79.
A. Kr?ner A. P. Willner E. Hegner A. Frischbutter J. Hofmann R. Bergner 《Geologische Rundschau》1995,84(3):437-456
Single zircons from two orthogneiss complexes, the Grey Gneiss and Red Gneiss, the lowermost tectonic units in the Erzgebirge, were dated. The grey Freiberg Gneiss is of igneous origin and has a 207Pb/206Pb emplacement age of 550±7 Ma. A quartz monzonite from Lauenstein contains idiomorphic zircons with a mean 207Pb/206Pb age of 555±7 Ma as well as xenocrysts ranging in age between 850 and 1910 Ma. Red gneisses from the central Erzgebirge contain complex zircon populations, including numerous xenocrysts up to 2464 Ma in age. The youngest, idiomorphic, zircons in all samples yielded uniform 207Pb/206Pb ages between 550±9 and 554±10 Ma. Nd isotopic data support the interpretation of crustal anatexis for the origin of both units. Nd(t) values for the grey gneisses are –7.5 and –6.0 respectively, (mean crustal residence ages of 1.7–1.8 Ga). The red gneisses have a wider range in Nd(t) values from –7.7 to –2.8 (T
DM ages of 1.4–1.8 Ga). The zircon ages document a distinct late Proterozoic phase of granitoid magmatism, similar in age to granitoids in the Lusatian block farther north-east. However, Palaeozoic deformation as well as medium pressure metamorphism ( 8 kbar/600–650° C) are identical in both gneiss units and distinguish these rocks from the Lusatian granitoids. The grey and red gneisses were overthrust by units with abundant high-pressure relicts and a contrasting P-T evolution. Zircon xenocryst and Nd model ages in the range 1000–1700 Ma are similar to those in granitoid rocks of Lusatia and the West-Sudetes, and document a pre-Cadomian basement in parts of east-central Europe that, chronologically, has similarities with the Sveconorwegian domain in the Baltic Shield. 相似文献
80.