首页 | 本学科首页   官方微博 | 高级检索  
文章检索
  按 检索   检索词:      
出版年份:   被引次数:   他引次数: 提示:输入*表示无穷大
  收费全文   1567篇
  免费   67篇
  国内免费   88篇
林业   65篇
农学   65篇
基础科学   21篇
  451篇
综合类   585篇
农作物   103篇
水产渔业   71篇
畜牧兽医   285篇
园艺   62篇
植物保护   14篇
  2024年   9篇
  2023年   14篇
  2022年   18篇
  2021年   31篇
  2020年   25篇
  2019年   33篇
  2018年   19篇
  2017年   55篇
  2016年   57篇
  2015年   63篇
  2014年   82篇
  2013年   76篇
  2012年   134篇
  2011年   144篇
  2010年   121篇
  2009年   107篇
  2008年   77篇
  2007年   111篇
  2006年   94篇
  2005年   56篇
  2004年   56篇
  2003年   49篇
  2002年   31篇
  2001年   23篇
  2000年   29篇
  1999年   27篇
  1998年   26篇
  1997年   20篇
  1996年   25篇
  1995年   28篇
  1994年   17篇
  1993年   11篇
  1992年   15篇
  1991年   5篇
  1990年   12篇
  1989年   10篇
  1988年   4篇
  1987年   6篇
  1986年   2篇
排序方式: 共有1722条查询结果,搜索用时 31 毫秒
1.
柑橘幼果发育期碳水化合物代谢及其与生长发育的关系   总被引:1,自引:0,他引:1  
温州蜜柑幼果在盛花后逐渐生长 盛花后6 d开始大量脱落 日本甜夏橙幼果在盛花后12 d内重量未增加,一直处于急剧落果期。甜夏橙幼果中蔗糖含量高出温州蜜柑20多倍,种间还原糖含量变化趋势略有不同。两种柑橘的淀粉含量变化也不同,但它们的淀粉含量与淀粉酶活性、幼果相对脱落率均呈负相关。对幼果碳水化合物代谢与生长、脱落的关系作了讨论。  相似文献   
2.
将12只2~3岁健康绵羊分为Ⅰ组(3只)、Ⅱ组(6只)和Ⅲ组(3只),分别按2.5,5.0,10.0 g/kg体重的剂量,向瘤胃内注入50%D—L消旋体乳酸溶液,各处理组均出现酸中毒症状.乳酸酸中毒时,肾脏的损伤程度与瘤胃内注入乳酸的剂量水平有关.各处理组瘤胃内注入乳酸后,尿素氮显著升高.第Ⅰ组尿液pH下降迅速,恢复亦快;第Ⅱ组尿液pH下降和回升均较缓慢,而且出现大量蛋白质和血液;第Ⅲ组尿液除见第Ⅰ、Ⅱ组的变化外,还出现肌红蛋白、酮体和尿胆素原.  相似文献   
3.
姜片虫虫体抗原氨基酸的测定   总被引:1,自引:0,他引:1  
本文报道4种方法制备姜片虫虫体抗原,进行氨基酸组成的测定。其氨基酸总量(mg/100ml)结果显示:Ag-F1:608.50;Ag-F2:645.80;Ag-F3:357.14;Ag-F4:501.40;以 Ag-F3总量为最低,但值得重视的是 Ag-F3的丙氨酸(8.34),组氨酸(8.60),甘氨酸(11.00);苏氨酸(12.00),均显著降低。而 Ag-F4的组氨酸(4.80)为17种氨基酸含量最低者。其原因有待探讨。  相似文献   
4.
套袋对红富士苹果色素及糖、酸含量的影响   总被引:58,自引:4,他引:58  
 以苹果(Malus pumila) ‘长富2’品种为试材, 研究了套袋对果皮色素及果肉糖、酸含量的影响。结果表明, 套袋果果皮色素、可溶性糖、可滴定酸具有同对照果基本相同的消长规律, 但含量均始终低于对照; 摘袋后果实可溶性糖含量迅速升高, 且花青苷积累速度明显快于对照; 套袋主要降低了果实中山梨醇和蔗糖的含量, 果糖和葡萄糖降低幅度相对较小。  相似文献   
5.
Estimating future fluxes of CH4 between land and atmosphere requires well-conceived process-based biogeochemical models. Current models do not represent the anaerobic oxidation of methane (AOM) in land surface soils, in spite of increasing evidence that this process is widespread. Our objective was to determine whether AOM, or potential AOM, commonly occurs in 20 hydromorphic soils spanning a wide range of chemical properties. Bulk soil samples were collected under shallow water near the shoreline of 15 recently drained fish ponds in southern Bohemia (Czech Republic), as well as from below the water table at 3 peatland locations in northeast Scotland and 2 acid sulfate soils on the southern coast of Finland. Each soil slurry was incubated under both oxic and anoxic conditions, with or without the addition of alternative electron acceptors (SO42− and NO3) or H2PO4. Here, “oxic” and “anoxic” conditions refer to anoxic soil respectively incubated in a headspace containing air or argon. Using the isotope dilution method, we determined the gross production and oxidation rates of CH4 after 2 days incubation under oxic headspace conditions, and after 2, 21 and 60 days incubation under anoxic conditions. Large differences in net CH4 fluxes were observed between soil types and between incubation conditions. AOM was detected in each of the 20 bulk soil samples, which spanned >6 pH units and 2 orders of magnitude in organic C content. Significant positive relationships were found between AOM and gross CH4 production rates under anoxic conditions, resulting in AOM rates that were sometimes higher than CH4 oxidation rates under oxic headspace conditions. There was no relationship between net and gross CH4 production rates, such that 2 soil types could display similar low net rates, yet conceal very large differences in gross rates. The effects of alternative electron acceptors on AOM were idiosyncratic and resulted in no net trend. We did find, however, a negative effect of SO42− and H2PO4 on gross CH4 production rates under anoxic and oxic conditions respectively. Under oxic headspace conditions, CH4 oxidation was related to soil organic C content. Taken collectively, our results suggest that AOM, or potential AOM, is prevalent over a wide range of soil types, that AOM may contribute substantially to CH4 oxidation in soils, and that AOM in soils should be integrated to current process-based CH4 cycling models.  相似文献   
6.
陈堞  林凯程  林沁  陈霞  陈鑫珠 《草地学报》2020,28(2):565-570
本试验旨在研究大米草(Spartina anglica Hubb.)中耐盐乳酸菌的分离鉴定及对大米草青贮品质的影响,以期为大米草青贮利用提供技术支持和理论依据。试验采用传统培养法筛选出耐盐浓度为10%的乳酸菌菌株,通过生理生化及16S rDNA序列分析法综合鉴定筛选的菌株,并将其添加到大米草原料中进行青贮效果观察。结果表明:分离获得的42株乳酸菌菌株,耐盐溶度最高为10%的4株乳酸菌均为同型发酵的植物乳杆菌(Lactobacillus plantarum),命名为C1、C2、C3和C4。4株乳酸菌均能提高大米草的青贮发酵品质,其中C4显著提高青贮料的可溶性碳水化合物和粗脂肪含量(P<0.05),显著降低青贮料的氨态氮含量(P<0.05);另外,C4处理组的干物质含量和乳酸含量显著高于其他3个菌株处理组(P<0.05),中性洗涤纤维、酸性洗涤纤维、半纤维素和丁酸含量显著(P<0.05)低于其他3个菌株处理组,青贮效果最佳。  相似文献   
7.
Ammonia oxidation, the first step of nitrification, is mediated by both ammonia-oxidizing archaea (AOA) and bacteria (AOB); however, the relative contributions of AOA and AOB to soil nitrification are not well understood. In this study we used 1-octyne to discriminate between AOA- and AOB-supported nitrification determined both in soil-water slurries and in unsaturated whole soil at field moisture. Soils were collected from stands of red alder (Alnus rubra Bong.) and Douglas-fir (Pseudotsuga menziesii Mirb. Franco) at three sites (Cascade Head, the H.J. Andrews, and McDonald Forest) on acidic soils (pH 3.9–5.7) in Oregon, USA. The abundances of AOA and AOB were measured using quantitative PCR by targeting the amoA gene, which encodes subunit A of ammonia monooxygenase. Total and AOA-specific (octyne-resistant) nitrification activities in soil slurries were significantly higher at Cascade Head (the most acidic soils, pH < 5) than at either the H.J. Andrews or McDonald Forest, and greater in red alder compared with Douglas-fir soils. The fraction of octyne-resistant nitrification varied among sites (21–74%) and was highest at Cascade Head than at the other two locations. Net nitrification rates of whole soil without NH4+ amendment ranged from 0.4 to 3.3 mg N kg−1 soil d−1. Overall, net nitrification rates of whole soil were stimulated 2- to 8-fold by addition of 140 mg NH4+-N kg−1 soil; this was significant for red alder at Cascade Head and the H.J. Andrews. Red alder at Cascade Head was unique in that the majority of NH4+-stimulated nitrifying activity was octyne-resistant (73%). At all other sites, NH4+-stimulated nitrification was octyne-sensitive (68–90%). The octyne-sensitive activity—presumably AOB—was affected more by soil pH whereas the octyne-resistant (AOA) activity was more strongly related to N availability.  相似文献   
8.
对多壁碳纳米管进行酸化处理,并采用原位聚合法制备了碳纳米管/聚氨酯复合材料。利用X射线光电子能谱分析(XPS)、电子扫描显微镜(SEM)、动态力学分析(DMA)研究了碳纳米管酸化与否对复合材料性能的影响。结果表明,碳纳米管经酸化处理后产生了羧基,碳纳米管的原位加入使得复合材料的储存模量和玻璃化转变温度都有所提高,而且经过酸化的碳纳米管对聚氨酯材料的改性要比未酸化碳纳米管对聚氨酯材料的改性效果更为显著。  相似文献   
9.
石榴果实的糖酸组成及风味特点   总被引:2,自引:0,他引:2  
采用高效液相色谱法测定4种石榴成熟期果实中糖和酸的组成,并对其味感值和糖酸组分与果实风味指标间的相关性进行分析。结果表明,石榴果实中可溶性糖组分有蔗糖、葡萄糖、果糖和山梨醇,其中葡萄糖和果糖含量最高,分别占总糖含量的43.84%~48.36%和49.18%~50.67%。4个品种中,"玉石籽"的总糖含量最高,"白皮"的最低。石榴果实中主要有机酸是奎宁酸、琥珀酸、草酸、L-苹果酸、莽草酸、柠檬酸和D-苹果酸,其中"玛瑙籽"的总酸含量最高,"青皮"的最低。石榴果实中果糖的味感值最大、其次是葡萄糖;味感值最大的酸是奎宁酸,其次为柠檬酸。相关性分析结果表明,石榴果实的糖酸比与甜味/酸味比值之间呈极显著正相关,各品种间糖酸比(甜味/酸味比值)的差异主要取决于有机酸的含量,与糖含量无关。综合其风味特点,"青皮"和"玉石籽"是甜味较浓的品种,"白皮"和"玛瑙籽"则是酸味较浓的品种。  相似文献   
10.
Fungal N2O production results from a respiratory denitrification that reduces NO3/NO2 in response to the oxidation of an electron donor, often organic C. Despite similar heterotrophic nature, fungal denitrifiers may differ from bacterial ones in exploiting diverse resources. We hypothesized that complex C compounds and substances could favor the growth of fungi over bacteria, and thereby leading to fungal dominance for soil N2O emissions. Effects of substrate quality on fungal and bacterial N2O production were, therefore, examined in a 44-d incubation after soils were amended with four different substrates, i.e., glucose, cellulose, winter pea, and switchgrass at 2 mg C g−1 soil. During periodic measurements of soil N2O fluxes at 80% soil water-filled pore space and with the supply of KNO3, substrate treatments were further subjected to four antibiotic treatments, i.e., no antibiotics or soil addition of streptomycin, cycloheximide or both so that fungal and bacterial N2O production could be separated. Up to d 8 when antibiotic inhibition on substrate-induced microbial activity and/or growth was still detectable, bacterial N2O production was generally greater in glucose- than in cellulose-amended soils and also in winter pea- than in switchgrass-amended soils. In contrast, fungal N2O production was more enhanced in soils amended with cellulose than with glucose. Therefore, fungal-to-bacterial contribution ratios were greater in complex than in simple C substrates. These ratios were positively correlated with fungal-to-bacterial activity ratios, i.e., CO2 production ratios, suggesting that substrate-associated fungal or bacterial preferential activity and/or growth might be the cause. Considering substrate depletion over time and thereby becoming limited for microbial N2O production, measurements of soil N2O fluxes were also carried out with additional supply of glucose, irrespective of different substrate treatments. This measurement condition might lead to potentially high rates of fungal and bacterial N2O production. As expected, bacterial N2O production was greater with added glucose than with added cellulose on d 4 and d 8. However, this pattern was broken on d 28, with bacterial N2O production lower with added glucose than with added cellulose. In contrast, plant residue impacts on soil N2O fluxes were consistent over 44-d, with greater bacterial contribution, lower fungal contribution, and thus lower fungal-to-bacterial contribution ratios in winter pea- than in switchgrass-amended soils. Real-time PCR analysis also demonstrated that the ratios of 16S rDNA to ITS and the copy numbers of bacterial denitrifying genes were greater in winter pea- than in switchgrass-amended soils. Despite some inconsistency found on the impacts of cellulose versus glucose on fungal and bacterial leading roles for N2O production, the results generally supported the working hypothesis that complex substrates promoted fungal dominance for soil N2O emissions.  相似文献   
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号