全文获取类型
收费全文 | 124篇 |
免费 | 5篇 |
国内免费 | 40篇 |
出版年
2024年 | 1篇 |
2023年 | 1篇 |
2022年 | 2篇 |
2020年 | 2篇 |
2019年 | 3篇 |
2018年 | 2篇 |
2017年 | 2篇 |
2016年 | 1篇 |
2015年 | 5篇 |
2014年 | 8篇 |
2013年 | 13篇 |
2012年 | 8篇 |
2011年 | 13篇 |
2010年 | 2篇 |
2009年 | 4篇 |
2008年 | 7篇 |
2007年 | 8篇 |
2006年 | 9篇 |
2005年 | 7篇 |
2004年 | 9篇 |
2003年 | 2篇 |
2002年 | 7篇 |
2001年 | 5篇 |
2000年 | 6篇 |
1999年 | 4篇 |
1998年 | 2篇 |
1997年 | 2篇 |
1996年 | 3篇 |
1995年 | 2篇 |
1994年 | 4篇 |
1993年 | 5篇 |
1992年 | 6篇 |
1991年 | 1篇 |
1989年 | 2篇 |
1988年 | 2篇 |
1987年 | 1篇 |
1984年 | 1篇 |
1983年 | 2篇 |
1976年 | 1篇 |
1970年 | 1篇 |
1959年 | 1篇 |
1957年 | 1篇 |
1956年 | 1篇 |
排序方式: 共有169条查询结果,搜索用时 15 毫秒
31.
32.
土壤含水量对桔小实蝇蛹期存活的影响 总被引:6,自引:0,他引:6
浸水时间、土壤含水量对桔小实蝇Bactroceradorsalis(Hendel)蛹的存活及成虫羽化的影响的研究结果表明:(1)不同浸水时间对桔小实蝇蛹存活率的影响不同。浸水时间越长,蛹存活率越低;浸水对初期蛹的影响较大,蛹龄越大,浸水作用效果越低。浸水时间(TW)、蛹期(AP)和蛹存活率(SP)之间关系符合以下模型:SP=0.4165-0.00307TW+0.2290AP-0.00004496T2W-0.0002528A2P+0.00008258TWAP。(2)土壤含水量对桔小实蝇成虫羽化影响明显。当土壤含水量较低或较高时,羽化率都明显受到抑制。相对含水量在30%~80%之间,蛹的羽化率较高。相对含水量(Ws)和成虫羽化率(E)之间存在以下关系:E=0.396+0.01985W-0.000181W2。 相似文献
33.
目的通过建立一个适应于尖吻蝮仔蛇生长发育的稳定的多功能生态系统的人工模拟生态养殖蛇场,以最大限度地降低仔蛇的饲料成本,从而达到降低人工养殖尖吻蝮蛇的成本。方法选取一个室外围墙式养蛇场作为试验基地。设计为适应于蛇、蛙、昆虫、蚯蚓、小杂鱼等动物生长繁衍的人工模拟生态环境,建立一个稳定的多功能蛇场生态系统,以尖吻蝮蛇100条,在试验以前随机抽取10条测量其体重和体长,并以活体动物饲料喂养法和科学饲养管理法进行试验养殖,并在进入第一、第二次冬眠前均随机抽取10条蛇仔测其体重和体长。结果本次试验与本蛇场室内人工饲养尖吻蝮仔蛇相比,不仅在体重、体长和肥满度方面均相差不大,而且仔蛇的存活率还有所提高。结论表明该人工模拟生态养殖蛇场能够满足尖吻蝮仔蛇生长发育的需要,达到了预期的目的。 相似文献
34.
Mesenchymal stromal cell (MSC) therapies have demonstrated therapeutic efficacy in a wide-ranging array of tissue injury and disease indications. An important aspect of MSC-mediated therapeutic activities is immune modulation. Consistent with the concentration of MSC therapeutic potency in its secretion, a significant proportion of MSC immune potency resides in the small extracellular vesicles (sEVs) secreted by MSCs. These sEVs, which also include exosomes, carry a large cargo enriched in proteins with potent immunomodulatory activities. They have been reported to exert potent effects on humoral and cellular components of the immune system in vitro and in vivo, and may have the potential to support the diametrically opposite pro- and anti-inflammatory functions necessary for tissue repair and regeneration following injury. Following injury, pro-inflammatory activities are necessary to neutralize injury and remove dead or injured tissue, while anti-inflammatory activities to facilitate migration and proliferation of reparative cell types and to increase vascularization and nutrient supply are necessary to repair and regenerate new tissue. Therefore, a critical immunomodulatory requisite of MSC sEVs in tissue regeneration is the capacity to support the appropriate immune activities at the appropriate time. Here, we review how some of the immune regulatory targets of MSC sEVs could support the dynamic immunomodulatory activities during tissue repair and regeneration. 相似文献
35.
本工作观察到10-6—10-5mol/L去甲肾上腺素(NE)和10-7—10-5mol/L异丙基肾上腺素(ISO)可明显促进离体培养的血管平滑肌细胞(VSMC)的增殖和DNA的合成,并呈剂量依赖效应,该效应可为相应的受体阻断剂phentolamine(10-6mol/L)和proptanolol(10-5mol/L)所抑制;nifedipine(10-6mol/L)和veraromil(10-6mol/L)分别与同样浓度的NE同时加入细胞培养液中,其细胞计数和3H-TdR掺入率分别较单用NE时显著降低(P<0.01),nifedipine与verapamil亦明显抑制ISO促VSMC增殖的作用。 相似文献
36.
37.
R. KELMAN WIEDER KIMBERLI D. SCOTT KATHERINE KAMMINGA MELANIE A. VILE DALE H. VITT† TIFFANY BONE† BIN XU† BRIAN W. BENSCOTER† JAGTAR S. BHATTI‡ 《Global Change Biology》2009,15(1):63-81
Boreal peatland ecosystems occupy about 3.5 million km2 of the earth's land surface and store between 250 and 455 Pg of carbon (C) as peat. While northern hemisphere boreal peatlands have functioned as net sinks for atmospheric C since the most recent deglaciation, natural and anthropogenic disturbances, and most importantly wildfire, may compromise peatland C sinks. To examine the effects of fire on local and regional C sink strength, we focused on a 12 000 km2 region near Wabasca, AB, Canada, where ombrotrophic Sphagnum‐dominated bogs cover 2280 km2 that burn with a fire return interval of 123±26 years. We characterized annual C accumulation along a chronosequence of 10 bog sites, spanning 1–102 years‐since‐fire (in 2002). Immediately after fire, bogs represent a net C source of 8.9±8.4 mol m−2 yr−1. At about 13 years after fire, bogs switch from net C sources to net C sinks, mainly because of recovery of the moss and shrub layers. Subsequently, black spruce biomass accumulation contributes to the net C sink, with fine root biomass accumulation peaking at 34 years after fire and aboveground biomass and coarse root accumulation peaking at 74 years after fire. The overall C sink strength peaks at 18.4 mol C m−2 yr−1 at 75 years after fire. As the tree biomass accumulation rate declines, the net C sink decreases to about 10 mol C m−2 yr−1 at 100 years‐since‐fire. We estimate that across the Wabasca study region, bogs currently represent a C sink of 14.7±5.1 Gmol yr−1. A decrease in the fire return interval to 61 years with no change in air temperature would convert the region's bogs to a net C source. An increase in nonwinter air temperature of 2 °C would decrease the regional C sink to 6.8±2.3 Gmol yr−1. Under scenarios of predicted climate change, the current C sink status of Alberta bogs is likely to diminish to the point where these peatlands become net sources of atmospheric CO2‐C. 相似文献
38.
39.
40.