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1.
天津滨海盐土的脱盐碱化及其防治   总被引:10,自引:0,他引:10  
天津滨海盐土在长期治理过程中由于盐土的脱盐碱化,以及缺少有机肥料和低矿化(高钠)碱性水灌溉等原因,已出现了程度不等的碱化土壤。试验表明,应用有机无机改土剂和增施有机肥、深耕深翻、咸淡水混合灌溉等农艺措施,并与工程措施、生物措施相结合进行综合治理,能收到明显的改良效果。  相似文献   
2.
为明确改良剂在苏打盐化草甸土不同深度土层的改良效果,采用室内淋溶土柱的试验方法,设置S0、S1、S2、S3、S4和S5(每个土柱横截面积0.0113 m~2)分别施用改良剂0.00、0.01、0.05、0.10、0.50 g和1.00 g,折合成公顷用量分别为0.0、8.9、44.3、88.5、442.5 kg·hm~(-2)和885.1 kg·hm~(-2))6个处理,分析淹水条件下不同改良剂用量对苏打盐化草甸土的洗盐效应。结果表明,与未施改良剂处理(S0)相比,S3、S4和S5处理显著降低不同土层(0~30cm)土壤容重(降幅3.88%~8.87%)、增加土壤孔隙度(增幅3.82%~9.38%)、降低土壤pH值(降幅2.36%~8.05%);S2、S3、S4和S5处理显著提高20~40 cm土壤水分入渗量,增幅55.9%~294.6%(P0.05);施用改良剂处理交换性Na~+含量在0~10 cm和10~20 cm土层显著降低,降幅4.84%~56.5%(P0.05),20~30 cm和30~40 cm土层中增幅1.09%~17.1%;S3、S4和S5处理0~10 cm土层电导率显著降低,降幅49.0%~60.4%(P0.05),20~40 cm土层显著增加,增幅3.68%~19.8%(P0.05);S2、S3、S4、S5处理10~20 cm土层碳酸根含量显著降低,降幅5.98%~23.4%(P0.05),S3、S4、S5处理0~30 cm土层碳酸氢根含量降幅1.49%~18.0%;S2、S3、S4和S5处理显著提高0~30 cm≥0.25 mm水稳性团聚体,增幅达16.4%~161.7%(P0.05);S3、S4和S5处理0~30 cm土层MWD显著增加,增幅达5.78%~161.7%(P0.05)。针对本次供试土壤盐渍化程度,综合改良效果及改良剂施用量,改良剂适宜用量为每个土柱0.10 g(88.5 kg·hm~(-2))(S3处理),可达到最优淋洗效果。  相似文献   
3.
【目的】探讨绵阳市水稻青立病发病原因和防治措施。【方法】采取调查分析与田间试验的方法,比较不同除草剂处理水稻青立病发病情况,测定发病田块土壤和水稻植株重金属种类及含量,初步明确绵阳市水稻青立病发病原因;分析不同防治手段下水稻青立病发病情况,探索水稻青立病防治措施。【结果】施用除草剂不会引起水稻青立病发生,但过量施用会显著降低稻谷产量。与不发病田块相比,发病田块 0~50 cm 土层重金属砷含量增加 2.3~5.6 mg/kg;与不发病植株相比,发病水稻植株总砷含量增加 0.03~0.20 mg/kg;与对照相比,在小麦季随整地施用硫磺并在水稻季随整地施用石灰可降低水稻青立病发病率 20.74%;与种植籼稻品种相比,在水稻青立病易发病田块种植粳稻品种可使发病率显著降低。【结论】绵阳市水稻青立病发生原因为土壤重金属砷、镉和铜含量偏高。苄乙、吡嘧磺隆、二氯喹啉酸和五氟磺草胺 4 种除草剂施用不是水稻青立病的发病原因。在麦稻轮作和秸秆全量还田条件下,在小麦季随整地施用硫磺并在水稻季随整地施用石灰对水稻青立病防治效果显著。  相似文献   
4.
生石灰是水产养殖的一种常规药物,非常普遍的用在水质消毒,疾病防治中,许多水产养殖用户也把生石灰作为一种常用的水质改良剂,但在甲鱼的养殖中,要根据情况酌情使用,否则,会出现pH值过高从而导致有毒气体的产生,造成甲鱼中毒的病况。本文介绍了温室甲鱼养殖中生石灰使用不当引起的病况,并提出了相应解救措施。实验中采用了生石灰日常消毒常用的浓度和间隔日期,伴随着pH值与氨氮的浓度升高,甲鱼出现了死亡现象,在解除了生石灰的使用后,甲鱼停止了死亡现象。  相似文献   
5.
秸秆还田是我国培肥地力和增加农田土壤碳固定的重要措施,但进入农田的秸秆存在着活化土壤重金属的风险。为了解不同来源的秸秆对污染水平不同农田土壤重金属活性的影响,采取相应措施防止因秸秆还田对农田土壤重金属的激活,开展了盆栽和田间小区试验研究秸秆还田配施石灰对水田土壤铜、锌、镉、铅活性的影响。盆栽和田间试验在轻度和重度污染2种土壤上同时进行。盆栽试验中施用秸秆包括重污染水稻秸秆、轻污染水稻秸秆和轻污染油菜秸秆3种,石灰用量设对照(0 kg·hm-2)和石灰处理(750 kg·hm-2)2个处理;田间小区试验设对照(不施秸秆和石灰)、秸秆还田及秸秆还田+石灰3个处理。动态观察了试验过程中土壤有效态重金属、重金属形态及水稻籽粒中重金属积累情况。结果表明,试验初期(前20 d)秸秆还田显著增加了水田土壤中水溶性有机碳与水溶性重金属的含量;与对照处理比较,水溶性重金属含量以重度污染土壤增幅较为明显。试验后期(60 d后)秸秆还田对土壤重金属的活性的影响逐渐变得不明显。油菜秸秆还田土壤中水溶性重金属含量低于水稻秸秆还田,重污染水稻秸秆还田土壤中水溶性重金属含量高于低污染水稻秸秆还田。盆栽试验和田间试验的结果都表明,重污染水稻秸秆还田可轻微增加水稻籽粒中镉的积累,但轻度污染水稻秸秆还田与油菜秸秆还田对水稻籽粒镉积累的影响较小;3种秸秆还田对水稻籽粒铅、铜、锌积累的影响不明显。配施石灰可显著降低土壤中水溶性重金属的含量,降低水稻籽粒中重金属的积累。研究认为,在污染农田管理上应控制重污染水稻秸秆还田,在秸秆还田的同时适量配施石灰。  相似文献   
6.
Abstract

Loss of soil‐water saturation may impair growth of rainfed lowland rice by restricting nutrient uptake, including the uptake of added phosphorus (P). For acidic soils, reappearance of soluble aluminum (Al) following loss of soil‐water saturation may also restrict P uptake. The aim of this study was to determine whether liming, flooding, and P additions could ameliorate the effects of loss of soil‐water saturation on P uptake and growth of rice. In the first pot experiment, two acid lowland soils from Cambodia [Kandic Plinthaqult (black clay soil) and Plinthustalf (sandy soil)] were treated with P (45 mg P kg?1 soil) either before or after flooding for 4 weeks to investigate the effect of flooding on effectiveness of P fertilizer for rice growth. After 4 weeks, soils were air dried and crushed and then wet to field capacity and upland rice was grown in them for an additional 6 weeks. Addition of P fertilizer before rather than after flooding depressed the growth of the subsequently planted upland rice. During flooding, there was an increase in both acetate‐extractable Fe and the phosphate sorption capacity of soils, and a close relationship between them (r2=0.96–0.98). When P was added before flooding, Olsen and Bray 1‐extractable P, shoot dry matter, and shoot P concentrations were depressed, indicating that flooding decreased availability of fertilizer P. A second pot experiment was conducted with three levels of lime as CaCO3 [to establish pH (CaCl2) in the oxidized soils at 4, 5, and 6] and four levels of P (0, 13, 26, and 52 mg P kg?1 soil) added to the same two acid lowland rice soils under flooded and nonflooded conditions. Under continuously flooded conditions, pH increased to over 5.6 regardless of lime treatment, and there was no response of rice dry matter to liming after 6 weeks' growth, but the addition of P increased rice dry matter substantially in both soils. In nonflooded soils, when P was not applied, shoot dry matter was depressed by up to one‐half of that in plants grown under continuously flooded conditions. Under the nonflooded conditions, rice dry matter and leaf P increased with the addition of P, but less so than in flooded soils. Leaf P concentrations and shoot dry matter responded strongly to the addition of lime. The increase in shoot dry matter of rice with lime and P application in nonflooded soil was associated with a significant decline in soluble Al in the soil and an increase in plant P uptake. The current experiments show that the loss of soil‐water saturation may be associated with the inhibition of P absorption by excess soluble Al. By contrast, flooding decreased exchangeable Al to levels below the threshold for toxicity in rice. In addition, the decreased P availability with loss of soil‐water saturation may have been associated with a greater phosphate sorption capacity of the soils during flooding and after reoxidation due to occlusion of P within ferric oxyhydroxides formed.  相似文献   
7.
针对猪场污水厌氧处理出水的有机物浓度高,后续处理困难的问题,该试验对石灰混凝法处理猪场高浓度厌氧出水的效果进行了测试,并与氧化塘的处理效果进行比较分析。试验中选择了1g/L和5g/L两种石灰投加剂量,对沉淀1、2、3、4、5和6h的净化效果进行取样分析;并对氧化塘猪场污水处理工艺连续取样三天,分析处理效果。结果表明:石灰混凝法投加剂量为5g/L、沉淀时间为5h时,对COD的去除率高达57.8%,明显好于氧化塘的去除效果;但对氨氮的去除率低于氧化塘。石灰混凝法沉淀时间短,基建投资小,可作为猪场污水进入二级处理或深度处理工艺前的可选择性过渡工艺。  相似文献   
8.
In the Cerrado savanna region in Brazil, the effects of different land use on Oxisol aggregation were studied using laser diffraction grain size analyses. The topsoil of plowed systems had significantly lower amount of macroaggregates (2000–194 μm) and a significantly higher amount of soil in the microaggregate size and primary particle fraction (<76 μm) compared to pastures and the native Cerrado. In plowed systems low in soil organic carbon (SOC), lime had a negative effect on aggregate stability. Lime addition had no effect on topsoil aggregation in land use systems that were not plowed regularly and generally had a higher SOC content. For all the studied topsoils, pHKCl was positively correlated with the amount of clay dispersed after 3 h of shaking in water. SOC did not influence clay dispersion in the range of soils studied. In continuous cropping systems in the Cerrado region, with a combination of mechanical stress and low SOC, liming will cause an increase in small aggregates and primary particles and hence contribute to a destabilization of the soil structure.  相似文献   
9.
Huang  B.  Kuo  S.  Bembenek  R. 《Water, air, and soil pollution》2004,158(1):37-51
Although evaluations of the availability of cadmium (Cd) contaminants in phosphate fertilizers have been made, few have examined the transfer efficiency of Cd from fertilizers to plants, especially under field conditions. This 2-year field study determined the transfer of added Cd to lettuce (Lactuca sativa L.) (Royal Green) from a western phosphate rock (PR) and a triple superphosphate (TSP) as affected by liming and rate of fertilizer (or Cd) input. A readily soluble Cd salt, CdCl2, was included in the study for comparison. The cumulative amounts of Cd added from the fertilizers and CdCl2 over the 2-year period ranged from 0 to 1440 g ha–1. Lettuce yield increased with increasing TSP rates, but was unaffected by PR. Significant (P < 0.01) effects of Cd source and rate, lime, and year were found on Cd accumulation by lettuce. The transfer of the added Cd was consistently higher for CdCl2 than for the fertilizers regardless of lime rate. A contrasting year effect was also found between the two P fertilizers. In the second year of application, the Cd transfer efficiency increased in the soil treated with the PR, but decreased in the soil treated with the TSP. The Cd transfer efficiency for the plant was better measured with DTPA–Cd (r 2= 0.78 – 0.80) or CaCl2–Cd (r 2= 0.57 – 0.76) than with soil total Cd (r 2= 0.39 to 0.54) across all Cd sources and lime rates. This is because DTPA–Cd or CaCl2–Cd reflected the influences of the amount of Cd added, Cd source, and lime rate on Cd accumulation by the plant better than did the soil total Cd. Of the amount of Cd added from the fertilizers an average of 1.0% or less was accumulated in the harvested lettuce tissue. Applications of the fertilizers at high rates could result in increased Cd accumulation in the soil over time.  相似文献   
10.
石灰与有机物料配施对作物镉铅吸收的控制效果研究   总被引:16,自引:5,他引:16  
通过采用石灰(L)、泥炭(P)、猪粪(M)、石灰 泥炭(LP)、石灰 猪粪(LM)等处理对福建省龙岩市新罗区特钢厂附近污染田进行改良的田问定位试验。表明大部分处理能提高土壤的pH值、有机质含量。处理石灰、石灰 泥炭和石灰 猪粪对提高作物产量均有显著效果。大部分处理能抑制水稻、花生对Cd、Pb的吸收,糙米中Pb的含量在食品卫生标准范围内。说明通过调节土壤pH值,改变土壤重金属活性是有机—中性化改良技术的主要机理。  相似文献   
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