全文获取类型
收费全文 | 11246篇 |
免费 | 2077篇 |
国内免费 | 4397篇 |
出版年
2023年 | 407篇 |
2022年 | 468篇 |
2021年 | 542篇 |
2020年 | 711篇 |
2019年 | 770篇 |
2018年 | 678篇 |
2017年 | 733篇 |
2016年 | 658篇 |
2015年 | 677篇 |
2014年 | 675篇 |
2013年 | 861篇 |
2012年 | 687篇 |
2011年 | 667篇 |
2010年 | 479篇 |
2009年 | 674篇 |
2008年 | 581篇 |
2007年 | 745篇 |
2006年 | 643篇 |
2005年 | 632篇 |
2004年 | 537篇 |
2003年 | 551篇 |
2002年 | 467篇 |
2001年 | 413篇 |
2000年 | 354篇 |
1999年 | 366篇 |
1998年 | 273篇 |
1997年 | 276篇 |
1996年 | 271篇 |
1995年 | 247篇 |
1994年 | 235篇 |
1993年 | 195篇 |
1992年 | 179篇 |
1991年 | 143篇 |
1990年 | 153篇 |
1989年 | 146篇 |
1988年 | 116篇 |
1987年 | 88篇 |
1986年 | 67篇 |
1985年 | 60篇 |
1984年 | 53篇 |
1983年 | 18篇 |
1982年 | 68篇 |
1981年 | 39篇 |
1980年 | 32篇 |
1979年 | 28篇 |
1978年 | 8篇 |
1977年 | 10篇 |
1975年 | 7篇 |
1973年 | 7篇 |
1958年 | 8篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
1.
黄土丘陵区生物土壤结皮表面糙度特征及影响因素 总被引:1,自引:0,他引:1
地表糙度是影响地表径流和侵蚀过程的重要属性.生物结皮在干旱半干旱区广泛分布,是地表糙度的影响因子之一.本文采用链条法测定了黄土丘陵区不同发育阶段生物结皮表面糙度特征,分析了不同发育阶段生物结皮表面糙度对坡向、土壤含水量和冻融作用的响应及其与各理化性质的相关性,初步探索了生物结皮对地表糙度的影响及其相关因素.结果表明: 生物结皮显著改变地表糙度,随着生物结皮从藻结皮向藓结皮演替,其糙度先降低后增加,生物结皮发育形成10年以后,其表面糙度基本趋于稳定;研究区早期形成的藻结皮表面糙度较裸土降低47.0%,深色藻结皮(藓类盖度<20%)较裸土降低20.4%,混生结皮(藓类盖度为20%~60%)和苔藓结皮(藓类盖度>70%)表面糙度与深色藻结皮基本一致;坡向对发育10年以上的生物结皮表面糙度的影响不显著;土壤含水量影响地表糙度特征.研究区浅色藻结皮表面糙度随水分变化较为剧烈;随着生物结皮发育,深色藻结皮、混生结皮和苔藓结皮表面糙度随水分的变化趋于平缓.冻融增加了生物结皮表面糙度.浅色藻结皮经两次冻融后表面糙度增加29.7%;深色藻结皮、混生结皮和藓结皮表面糙度的影响需经过反复冻融才有所体现.生物结皮表面糙度与藓结皮盖度呈显著正相关(P<0.1). 相似文献
2.
尽管国内外对养殖污水处理已提出了一系列的工艺技术,但因经济原因养殖污水直接灌溉农田在我国农村地区仍较为常见.为了解长期畜禽养殖污水直灌对稻田土壤质量的影响,在浙江省绍兴市柯桥区选择了养殖污水直灌不同年限(0、4、7、13年)的稻田,比较研究了养殖污水直接灌溉对稻田土壤不同深度土层中各形态氮和磷含量的影响,探讨了长期养殖污水灌溉对氮、磷在土壤剖面中垂直迁移的影响.结果表明: 长期养殖污水直接灌溉可显著提高稻田土壤中氮和磷的积累,积累量随灌溉年限的增长而增加,其中磷素的增幅高于氮素.养殖污水灌溉4、7和13年后,土壤表层中全P和全N分别比对照增加了43.6%、95.2%、1484%和7.7%、17.0%、28.4%.土壤氮素的变化为NH4+-N、NO3--N>酸解有机氮>非酸解有机氮;土壤有效磷的变化明显大于全磷.长期养殖污水灌溉可促进氮、磷在土壤剖面中的垂直迁移,增加对地下水的污染风险.
相似文献
3.
An ecosystems approach to base-rich freshwater wetlands,with special reference to fenlands 总被引:1,自引:1,他引:0
Geert van Wirdum 《Hydrobiologia》1993,265(1-3):129-153
A survey of base-rich wetlands in The Netherlands is presented. The main area of their occurrence is the low-lying Holocene
part of the country, until some thousand years ago a large and coherent wetland landscape: the Holland wetland. The development
of various parts of the Holland wetland into marshes, fens and bogs can be understood from hydrological relations in mire
basins, as recognized in the distinction of primary, secondary and tertiary mire basin stages. Presently, the remnants of
the Holland wetland are separate base-rich wetlands. The succession of their vegetation reflects various abiotic conditions
and human influences. Three main developmental periods are distinguished as regards these factors. The first, geological period
of mire development is seen as a post-glacial relaxation, with the inertia due to the considerable mass of wetland as a stabilizing
factor. Biological “grazing” influences, as an aspect of utilization by humans, converted base-rich wetlands to whole new
types in the second, historical period. Presently, mass and harvesting have decreased in importance, and actual successions
in terrestrializing turbaries seem to reflect rapidly changing environmental conditions. Human control could well become the
most important factor in the future development of wetland nature. The present value of open fen vegetation strongly depends
on the continuation of the historical harvesting. The development of wooded fen may help to increase the mass of wetland in
the future. Best results in terms of biodiversity are expected when their base state is maintained through water management.
The vegetation and hydrology of floating fens in terrestrializing turbaries is treated in some more detail. Various lines
and phases in the succession are distinguished. Open fen vegetation at base-rich, yet nutrient-poor sites is very rich in
species threatened elsewhere. The fast acidification of certain such fens is attributed to hydrological and management factors.
This acidification is illustrated in the profile of a floating raft sample. At the scale of these small fens, the elemental
structure comprising base-rich fen, transitional fen and bog vegetation, is not as stable as it was in the large Holland wetland.
A critical role seems to be played by the supply of bases with the water influx. The changing base state is supposed to change
the nutrient cycling to such an extent that it would be correct to call this trophic excitation of the ecosystem, rather than
just eutrophication. Eutrophication indicates a quantitative reaction to an increased nutrient supply, the internal system
being unaltered. The drainage of fens, resulting in an increased productivity of the vegetation, provides another example
of excitation, to the effect that the functional system is dramatically changed internally. 相似文献
4.
茶园冬季乔木落叶的分解和矿质元素释放 总被引:1,自引:0,他引:1
在我国南方存在着一种传统植茶方式——茶林复合生态系统,近年来人们已逐步认识到它在维持土壤肥力,抗御自然灾害和保证茶叶内质特性等方面的作用,然而对冬季乔木落叶分解和矿质元素释放的作用尚无报道。本文是对安徽省黄山市休宁县茶树-乌桕复合园和茶树-板栗复合园的冬季乔木落叶分解的研究,为全面认识茶林复合生态系统的性质提供依据。 相似文献
5.
CO2 exchange between the atmosphere and soil algal crusts of the Trachypogon savannas of the Orinoco Llanos has been analyzed
using an open gas exchange system. These savannas encompass a wide range of physiognomic types, from herbaceous communities
to savanna woodlands. A maximum CO2 flux of 0.207 mg m-2 s-1 was measured in the crusts of the Guanipa savannas, while in the other examined crusts (0.035–0.105 mg m-2 s-1) the flux was similar to values reported for terrestrial algae. The CO2 flux data were statistically fitted to the photosynthetically active radiation by a logarithmic relationship, and the photosynthetic
efficiencies of the crusts were compared. The activation energy calculated for the CO2 fixation indicates that limitations by diffusion and photochemical processes were excluded in the Guanipa crusts (above 12
kcal mole-1), whereas they were evident in the other crust studied. An optimum CO2 incorporation as a function of the crust water potential was established and carbon gain strategies were proposed on the
basis of the results and characteristics of the habitats. 相似文献
6.
Spatial variability in nutrient concentrations in the intertidal sediments and pore waters has been studied along downshore
transects and in core profiles at three locations in the Shannon estuary on the west coast of Ireland. The parameters measured
were N, as Kjeldahl N, NO3, NO2, and NH3, and P as total P and PO4 along with a range of other environmental variables such as salinity and sediment organic content.
The concentrations of all nutrients varied with season, but winter values were generally low in comparison with polluted mainland
european estuaries. There was a great deal of variation in nutrient concentrations along the transects, and coefficients of
variability of up to 153% (NH3), 173% (NO3), 129% (NO2) and 117% (PO4) were found. Overall, there was little evidence of any trends in concentration in any of the nutrients from the top to the
bottom of the transects, although it was occasionally possible to link particular instances to local conditions such as the
presence of the channel or a stream.
Sediment core profiles showed typical patterns, with NO3 concentrations for example being highest in surface sediments, while NH3 and PO4 concentrations increased with depth. Rather surprisingly perhaps, NO3 could still be detected on occasion at depths of up to 20 cm, well below the Redox Potential Discontinuity (RPD) and the
limit of oxygen penetration which oxygen microelectrodes had measured as being within a few mm of the surface. This was ascribed
to the activities of the macrofauna, in that the oxidised sediment which lined the burrows could clearly be seen in some cores.
This study not only shows that nutrient distributions along estuarine gradients are linked to physicochemical factors such
as oxygenation and freshwater/marine influence, but also that sediment instability, through random physical events such as
storms, and macrofaunal activity play an important role and that these latter factors deserve closer attention. 相似文献
7.
Laboratory experiments have shown appreciable losses of ammonia after injection of anhydrous ammonia into dry and wet soils.
In this study losses of ammonia injected into a moist (tension 10 kPa), dry (tension 160 kPa) and a wet (tension 1.6 kPa)
sandy loam were measured under field conditions using wind tunnels. Losses were insignificant from a moist soil. However losses
from a dry and a wet soil were 20% and 50% of injected ammonia, respectively. From the dry soil, losses of gaseous ammonia
took place within the first hours after injection, which indicates a rapid transport through cracks and voids. From the wet
soil, 20% of the injected ammonia was lost more gradually between 6 h and 6 d. This indicates that upward movement of water
due to evaporation may be the cause of these ammonia losses which proceeded for longer periods. 相似文献
8.
Abstract. Maintenance of realistically low solution P concentrations under controlled conditions is a major difficulty in studies of P nutrition. In this report, we describe a relatively simple and economical sand culture system capable of sustaining plant growth to maturity under controlled yet realistic P regimes. The system uses Al2 O3 as a solid-phase P buffer, and modern process control technology to control irrigation and addition of other mineral nutrients. Aspects of the design, use and potential applications of automated solid-phase systems are discussed. The system was used to grow Phaseolus vulgaris to matarity at 0.4 mmol m3 , 1.0 mmol m3 and 27 mmol m3 P with and without mycorrhizal inoculation. At flowering, low solution P concentrations were associated with reduced leaf concentrations of P in nonmycorrhizal plants, and reduced leaf concentrations of Ca in both mycorrhizal and nonmycorrhizal plants. Mycorrhizal inoculation increased leaf P, K, Mg and Mn concentrations, but reduced leaf N concentration. Low P regimes reduced final seed yield by diminishing both the number of pods per plant and the number of seeds per pod. Mycorrhizal inoculation significantly enhanced seed yield under low P regimes by increasing seed weight, the number of pods per plant, and the number of seeds per pod. 相似文献
9.
川西亚高山不同森林类型土壤呼吸和总硝化速率的季节动态 总被引:3,自引:0,他引:3
川西亚高山原始林及其采伐后通过不同恢复措施形成的不同类型森林土壤呼吸和总硝化速率的对比分析及其耦合关系的研究相对匮乏。采用气压过程分离系统(Ba PS)技术研究了川西亚高山岷江冷杉原始林及其砍伐后恢复的粗枝云杉阔叶林、红桦-岷江冷杉天然次生林和粗枝云杉人工林土壤呼吸和总硝化速率的季节动态及其影响因素。结果表明:生长季内平均土壤呼吸速率和总硝化速率分别以粗枝云杉阔叶林和粗枝云杉人工林较高,均以岷江冷杉原始林较低。土壤呼吸和总硝化速率在生长季内具有明显的季节动态,呈以7月份最高的单峰趋势。土壤呼吸和总硝化速率与土壤温度显著相关,而与土壤水分相关性不显著,表明土壤温度是调控呼吸和总硝化作用季节动态的主要因子。土壤呼吸的温度敏感性(Q_(10))介于2.59—4.71,以岷江冷杉原始林最高,表明高海拔的岷江冷杉原始林可能更易受到气候变化的影响。林型间土壤呼吸和总硝化速率主要受凋落物量、p H和有机质的影响。不同林型间土壤呼吸和总硝化速率显著正相关,表明土壤呼吸和总硝化速率存在耦合关系。 相似文献
10.
模拟增温对西藏高原高寒草甸土壤供氮潜力的影响 总被引:3,自引:0,他引:3
过去几十年青藏高原呈现显著的增温趋势,冬季增温幅度显著高于生长季的季节非对称特征。气候变暖会对生态系统氮素循环产生重要影响,但关于全年增温与冬季增温对高寒生态系统氮循环的不同影响仍缺乏研究。在青藏高原高寒草甸区开展模拟增温试验,研究季节非对称增温对高寒草甸生态系统氮循环的影响。该试验布设于2010年7月,设置3种处理(不增温、冬季增温与全年增温)。研究结果发现,开顶箱增温装置造成了小环境的暖干化:显著提高了地表空气温度和表层土壤温度,降低了表层土壤含水量。冬季增温会加剧土壤中氮素的流失,所以在经历了冬季增温后土壤氮含量显著降低;在生长季节,土壤氮素周转速率受土壤水分的调控,在降雨较少的季节,增温引起的土壤含水量降低会抑制土壤氮周转速率。对于土壤微生物量而言,高寒草甸土壤微生物量碳表现出明显的季节动态,在生长季旺盛期较低,在生长季末期和初冬季节反而较高,这说明为了降低对土壤养分的竞争,高寒草甸植物氮吸收与土壤微生物氮固持在时间上存在分离。研究结果表明,冬季增温导致的土壤养分含量变化会影响随后生长季植物群落的生产力、结构组成与碳氮循环等过程,对生态系统过程产生深远的影响。 相似文献