全文获取类型
收费全文 | 11195篇 |
免费 | 653篇 |
国内免费 | 1069篇 |
专业分类
林业 | 1456篇 |
农学 | 597篇 |
基础科学 | 385篇 |
4435篇 | |
综合类 | 4171篇 |
农作物 | 301篇 |
水产渔业 | 344篇 |
畜牧兽医 | 613篇 |
园艺 | 148篇 |
植物保护 | 467篇 |
出版年
2024年 | 186篇 |
2023年 | 427篇 |
2022年 | 504篇 |
2021年 | 499篇 |
2020年 | 480篇 |
2019年 | 562篇 |
2018年 | 419篇 |
2017年 | 634篇 |
2016年 | 749篇 |
2015年 | 620篇 |
2014年 | 717篇 |
2013年 | 915篇 |
2012年 | 983篇 |
2011年 | 908篇 |
2010年 | 623篇 |
2009年 | 579篇 |
2008年 | 475篇 |
2007年 | 511篇 |
2006年 | 437篇 |
2005年 | 348篇 |
2004年 | 256篇 |
2003年 | 176篇 |
2002年 | 131篇 |
2001年 | 127篇 |
2000年 | 95篇 |
1999年 | 92篇 |
1998年 | 87篇 |
1997年 | 46篇 |
1996年 | 48篇 |
1995年 | 52篇 |
1994年 | 36篇 |
1993年 | 38篇 |
1992年 | 32篇 |
1991年 | 19篇 |
1990年 | 31篇 |
1989年 | 18篇 |
1988年 | 14篇 |
1987年 | 10篇 |
1986年 | 9篇 |
1985年 | 6篇 |
1984年 | 7篇 |
1982年 | 2篇 |
1980年 | 1篇 |
1979年 | 2篇 |
1978年 | 5篇 |
1977年 | 1篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
11.
采用二因素裂区设计,以保水剂和活性炭、硅藻土、凹凸棒为填充剂的包衣材料制作丸粒化胡麻种子,研究了丸粒化处理对胡麻种子萌发和幼苗生长的影响。结果表明:与不加保水剂相比,保水剂质量与种子质量为1∶1时,丸粒种子的活力指数和出苗率显著提高20.11%、18.62%;随着保水剂含量的增加,幼苗的根冠比显著减小3.25%。包衣剂中以活性炭:凹凸棒=1∶1为填充剂的发芽率和出苗率比不加填充剂的明显提高6.79%、22.41%,幼苗生长最健壮。与未丸粒化的种子相比,当保水剂质量与种子质量为1∶1时,以活性炭:凹凸棒=1∶1为填充剂的丸粒种子发芽指数、活力指数和出苗率显著提高,而且幼苗的茎粗、叶面积和根冠比分别显著增加11.02%、27.35%、28.07%。可见,适量的保水剂(保水剂质量与种子质量为1∶1)和以活性炭、凹凸棒为填充剂的包衣剂能提高胡麻种子活力,增加出苗率,使幼苗的干物质重增大,根系发达,根冠比提高,为胡麻高产奠定了良好的基础。 相似文献
12.
M. Yaeesh Siddiqi Bhupinder Malhotra Xiangjia Min Anthony D. M. Glass 《植物养料与土壤学杂志》2002,165(2):191-197
Effects of varying the proportions of NO3— and NH4+ in the growth medium on seedling growth and tomato fruit yield (Lycopersicon esculentum L. cv. Trust F1) were investigated in greenhouse hydroponic experiments. The presence of NH4+ as the sole N source (11 mM) was toxic: it curtailed growth and decreased chlorophyll content of the leaves. However, at low concentration (10 % of total N), the presence of NH4+, with or without added dissolved inorganic carbon (DIC), increased vegetative growth and fruit yield by ˜ 15 %, and enhanced taste/flavor of the fruits. In DIC‐enriched treatment, pH was maintained at 5.8 by addition of KHCO3 or as CaCO3. The presence of NH4+, at 10 % of total N, inhibited NO3— uptake rates by ˜ 27 %. The rates of uptake of NO3— and NH4+ were comparable (13.3 and 14.2 mmol plant—1 d—1, respectively, in the presence of DIC, and 14.7 and 14.0 mmol plant—1 d—1, respectively, in the absence of DIC), despite such a large difference in their concentrations in the nutrient feed solution. A higher proportion of NH4+ (up to 50 % of total N) had no further significant effect upon early vegetative growth, but in a long‐term experiment resulted in a high incidence of blossom end‐rot (BER) disease, thereby severely curtailing fruit yield. The presence of even 1.1 mM NH4+ reduced Ca2+ and Mg2+ accumulation in the leaves as well as in fruits. 相似文献
13.
宁夏回族自治区平罗县主要农作物碳足迹研究 总被引:2,自引:0,他引:2
农田碳足迹可以全面地反映农作物生产过程中各种因素引起的碳排放效应,是指导农业生产节能减排的重要指标。为探明农作物生产的碳足迹,基于宁夏回族自治区平罗县农田生产的实地调查数据,利用碳足迹的基本理论和方法,测算了该县农作物碳足迹。结果表明,水稻、玉米和小麦的碳足迹分别为1 487.56±164.59,913.03±142.99和809.75±144.99kg Ce/(hm2.a);碳成本分别为0.17±0.05,0.08±0.02g和0.12±0.03kg Ce/kg;化肥的施用量是影响碳足迹的主要因素,而水稻生产过程中灌溉水及育秧过程也是其碳足迹较高的主要原因。为了提高农田固碳减排增汇效益,应压缩水稻种植面积,扩大玉米和小麦种植,同时,建立节肥低碳高效的种植模式是实现平罗县农田节能减排的有效途径。 相似文献
14.
目的 明晰不同林分类型下土壤有机碳库特征,以期为平原沙土区土壤碳库的提高和生态恢复提供理论依据。 方法 以江苏省平原沙土区丰县16年生杨树纯林、柳树纯林、杨柳混交林3种林分类型及相邻的撂荒地(对照)为对象,测定0~20、20~40、40~60、60~80、80~100 cm等5个土壤层次有机碳及活性组分和土壤酶活性,计算土壤碳库管理指数,并对土壤有机碳库特征和环境因子进行相关性分析。 结果 (1)3种林分类型及对照各土层有机碳含量和储量范围分别为1.03~5.88 g·kg−1和3.53~17.55 t·hm−2。与对照相比,0~100 cm土层,3种林分类型土壤有机碳含量增加了45.2%~82.2%。杨树纯林0~100 cm土层有机碳储量分别是柳树纯林、杨柳混交林和对照的1.23、1.24、1.83倍。(2)与对照相比,0~100 cm土层,3种林分类型的土壤易氧化有机碳、可溶性有机碳和微生物生物量碳含量分别提高了28.6%~48.0%、6.8%~9.7%和21.6%~33.4%。3种林分类型土壤碳库管理指数显著高于100%(P<0.05)。(3)林分类型显著影响土壤蔗糖酶和多酚氧化酶活性(P<0.05),杨柳混交林0~100 cm土层多酚氧化酶活性显著高于杨树纯林和对照(P<0.05)。(4)相关性分析表明,土壤有机碳库特征受多酚氧化酶和β-葡萄糖苷酶活性显著影响,有机碳含量和储量、易氧化有机碳含量及碳库管理指数受蔗糖酶、过氧化物酶活性显著影响,微生物生物量碳受蔗糖酶活性显著影响。冗余分析表明,土壤碳氮比和细根生物量是土壤有机碳库特征的主要影响因素。 结论 平原沙土区营造人工林提高了土壤有机碳及活性组分和有机碳库稳定性,杨树纯林提高土壤有机碳储量效果最好。 相似文献
15.
Short term soil priming effects and the mineralisation of biochar following its incorporation to soils of different pH 总被引:2,自引:0,他引:2
The aim of this work was to determine the magnitude of the priming effect, i.e. short-term changes in the rate (negative or positive) of mineralisation of native soil organic carbon (C), following addition of biochars. The biochars were made from Miscanthus giganteus, a C4 plant, naturally enriched with 13C. The biochars were produced at 350 °C (biochar350) and 700 °C (biochar700) and applied with and without ryegrass as a substrate to a clay-loam soil at pH 3.7 and 7.6. A secondary aim was to determine the effect of ryegrass addition on the mineralisation of the two biochars.After 87 days, biochar350 addition caused priming effects equivalent to 250 and 319 μg CO2-C g−1 soil, in the low and high pH soil, respectively. The largest priming effects occurred at the start of the incubations. The size of the priming effect was decreased at higher biochar pyrolysis temperatures, which may be a way of controlling priming effects following biochar incorporation to soil, if desired. The priming effect was probably induced by the water soluble components of the biochar. At 87 days of incubation, 0.14% and 0.18% of biochar700 and 0.61% and 0.84% of biochar350 were mineralized in the low and high pH soil, respectively. Ryegrass addition gave an increased biochar350 mineralisation of 33% and 40%, and increased biochar700 at 137% and 70%, in the low and high pH soils, respectively. Certainly, on the basis of our results, if biochar is used to sequester carbon a priming effect may occur, increasing CO2-C evolved from soil and decreasing soil organic C. However, this will be more than compensated for by the increased soil C caused by biochar incorporation. A similar conclusion holds for accelerated mineralisation of biochar due to incorporation of fresh labile substrates. We consider that our results are the first to unequivocally demonstrate the initiation, progress and termination of a true positive priming effect by biochar on native soil organic C. 相似文献
16.
大气氮沉降的不断加剧,改变了土壤理化性质,直接影响植物的生长与发育,间接影响了陆地生态系统碳库,进而可能改变全球气候变化进程。森林是陆地生态系统的主体,因此,弄清氮沉降如何影响森林生态系统碳库,对预测全球气候变化具有重要意义。笔者旨在详细分析氮沉降对森林生态系统土壤碳库输入和输出的影响,阐述氮沉降对森林生态系统凋落物分解、细根周转和土壤呼吸的影响研究进展和作用机制。截至目前,关于氮沉降对于陆地生态系统的影响研究报道较多,且国内外诸多学者也在森林生态系统土壤碳库对氮沉降的响应领域开展了较多试验研究,但多集中于碳输入和输出的总量分析,而对输入和输出各个组分的研究相对较少。笔者综述了国内外有关森林生态系统碳库输入和输出各组分对氮沉降响应的相关研究,为进一步揭示其响应机制和途径提供参考依据。 相似文献
17.
18.
E. Weigand C. Boesch‐Saadatmandi 《Journal of animal physiology and animal nutrition》2013,97(4):710-719
The aim of the study was to compare apparent Zn absorption and Zn status of weanling rats fed diets that differed in Zn level, fat level and fat source. Semi‐synthetic diets, which were about isoenergetic and contained 3% soyabean oil, were supplemented with 7 or 100 mg Zn/kg to create a mild Zn deficiency (LZ) or a high Zn supply (HZ) and with 0 (LF), 22% beef tallow (BT) or 22% sunflower oil (SF) according to a 2 × 3 factorial design of treatments. They were fed ad libitum to 6 × 8 rats for 28 days. Energy intake and growth rates were comparable among the HZ groups. Weight gains in the LZ‐LF, LZ‐BT and LZ‐SF groups averaged 5.54, 4.95 and 4.15 g/day, and apparent Zn absorption averaged 79.4, 60.3 and 48.0 μg Zn/day, respectively, whereas faecal Zn excretion was comparable among these groups. Apparent Zn absorption, and plasma and femur Zn concentrations were lower in the high‐fat groups than in the LF group, possibly due to the high cellulose content of the BT and SF diets. Plasma Zn concentrations were higher in the animals fed the BT‐based than in the SF‐based diets, whereas femur and soft tissue Zn concentrations were comparable among these groups. The differences between the LZ‐BT and LZ‐SF groups in growth rate, Zn absorption rate and Zn status were confirmed in a second experiment. The results indicate that moderately Zn‐deficient diets enriched with SF in relation to BT affect Zn metabolism of weanling rats by a yet unknown mechanism. 相似文献
19.
试验以新鲜猪粪为发酵原料,研究湿法和干法两种不同厌氧发酵过程的碳、氮排放量。湿发酵和干发酵组发酵料液的总固体(TS)含量分别为8%和20%,发酵液pH为6.8~7.4,发酵温度为35℃,体积为1.2 L,周期为21 d。试验期间每天测产气量,每4天取发酵样,测其全氮含量和TS降解率。结果表明,湿法和干法发酵组的CH4总产气量分别为9114 mL和12537 mL;CO2的总产气量分别为251.90 mmol和343.67 mmol;TS降解率分别为52.5%和29%。湿发酵的碳流失率和全氮流失率极显著高于干发酵(P<0.05)。 相似文献
20.