施肥量对温室滴灌番茄干物质累积、产量及水肥利用的影响   总被引：2，自引：0，他引：2  

贾宋楠  范凤翠  刘胜尧  李志宏  赵楠  杜凤焕  张哲  王贺垒  贾建明  秦勇 《灌溉排水学报》2017,36(5)

为研究日光温室秋冬茬番茄生育时期干物质生产动态规律,探索高产高效的科学施肥模式,以标准冲施肥(含N量16%,含P_2O_5量5%,含K_2O量19%)为施肥种类,施肥量以N素为基准分为4个肥料处理水平,即F1(高肥)、F2(中肥)、F3(低肥)、F4(不追肥),分析了不同施肥量对日光温室番茄干物质累积、产量和水肥利用的影响。结果表明,番茄产量和水分利用效率(WUE)与施肥量呈"抛物线"关系,当N施量为290.6 kg/hm2(F2)时达到最高值,分别为67 776.93 kg/hm2和49.27 kg/m3,说明适量施肥可提高产量及水分利用效率。但肥料生产效率(PFP)在施肥量为(N)41.4~539.9 kg/hm2范围内呈现负指数降低趋势。植株干物质累积量表现出F2处理F1处理F3处理F4处理。果实干物质累积进程符合logistic函数轨迹,中肥处理比高肥、低肥处理提前进入快速累积期,使快速累积期持续时间比其他处理长1~8 d。全株总干物质转移量对果实贡献率为1.97%~6.96%,说明果实干物质高达90%以上依靠株体自身光合作用填充。因此,番茄结果期加强水肥的供给是必要的。  相似文献   

Influence of inorganic fertilizers and organic amendments on soil organic matter and soil microbial properties under tropical conditions   总被引：33，自引：0，他引：33  

Sneh Goyal  K. Chander  M. C. Mundra  K. K. Kapoor 《Biology and Fertility of Soils》1999,29(2):196-200

 Soil organic matter level, mineralizable C and N, microbial biomass C and dehydrogenase, urease and alkaline phosphatase activities were studied in soils from a field experiment under a pearl millet-wheat cropping sequence receiving inorganic fertilizers and a combination of inorganic fertilizers and organic amendments for the last 11 years. The amounts of soil organic matter and mineralizable C and N increased with the application of inorganic fertilizers. However, there were greater increases of these parameters when farmyard manure, wheat straw or Sesbania bispinosa green manure was applied along with inorganic fertilizers. Microbial biomass C increased from 147 mg kg^–1 soil in unfertilized soil to 423 mg kg^–1 soil in soil amended with wheat straw and inorganic fertilizers. The urease and alkaline phosphatase activities of soils increased significantly with a combination of inorganic fertilizers and organic amendments. The results indicate that soil organic matter level and soil microbial activities, vital for the nutrient turnover and long-term productivity of the soil, are enhanced by use of organic amendments along with inorganic fertilizers. Received: 6 May 1998  相似文献   

黄泛区潮土-冬小麦系统中尿素的转化和化肥氮去向   总被引：24，自引：5，他引：24  

张绍林  朱兆良  徐银华 《核农学报》1989,3(1):9-15

在田间条件下,用~(15)N标记的微区试验法研究了潮土-冬小麦系统中尿素的转化和化肥氮的去向。结果表明:土壤中尿素水解后,主要进行硝化和生物固定,而被粘土矿物固定的量很少;小麦返青后,随着气温上升,生物固定的标记氮不断分解,其量可达总生物固定量的60％。作为基肥条施的尿素,其损失略高于作返青肥或拔节肥表施后随即灌水的处理。氮素损失主要发生在春季气温回升后的生长期间,当季的淋洗损失极微。在较为适宜的用量和施用技术下,化肥氮的损失仍达33—45％,其中以碳酸氢铵为最高,次为硫酸铵和硝酸铵,而尿素和硝酸铵中的硝态氮损失最低。  相似文献   

保水剂与肥料互作及保水缓/控释肥料研究展望   总被引：9，自引：0，他引：9  

何绪生  廖宗文  黄培钊  葛仁山  李洪波  赵建华 《土壤通报》2006,37(4):799-804

保水剂在农业上的作用日益重要,肥料与保水剂一体化使用是水肥调控的重要技术,是肥料研究的国际前沿。保水剂是吸水量超过自身重量数百倍以上的亲水性高聚物。保水剂一般分为天然的,合成的及半合成的。保水剂与肥料可以通过物理混合、包膜或化学合成三种方式结合为一体化的保水缓/控释肥料。保水剂具有吸水吸肥功能,保水剂可吸附大量中性分子,对阳离子养分也有较强吸附作用,对阴离子养分吸附弱。肥料种类与盐浓度影响保水剂的吸附作用与膨胀能力。保水缓/控释肥料在土壤中对肥料养分有延迟释放作用。保水缓/控释肥料可改善土壤持蓄水分和水肥交互作用,促进植物对养分的吸收和作物增产。保水缓/控释肥料发展方向是包膜和化成保水缓/控释肥料。保水缓/控释肥料湿润及养分控释机理研究也需要加强。  相似文献   

长期施氮、磷、钾化肥对玉米产量及土壤肥力的影响   总被引：53，自引：3，他引：53  

刘恩科  赵秉强  胡昌浩  李秀英  李燕婷 《植物营养与肥料学报》2007,13(5):789-794

以1990年建立的国家褐潮土土壤肥力与肥料效益长期监测基地(北京昌平站)的长期肥料定位试验为研究平台,研究了不同施肥制度对玉米产量和土壤肥力的影响。结果表明,长期均衡地施NPK肥或NPK与有机肥配施,可以显著提高玉米产量和土壤有机质、全氮、全磷、速效氮、速效磷、速效钾等肥力指标,并能提高土壤微量元素的含量;而不均衡施肥(N、NK、NP、PK)导致相应的营养元素的耗竭。相关分析表明,在褐潮土上增施磷肥和有机肥对提高玉米产量具有重要的作用。  相似文献   

Nitrogen fertilizer–induced mineralization of soil organic C and N in six contrasting soils of Bangladesh     

Mohammad I. Khalil  Muhammad S. Rahman  Urs Schmidhalter  Hans‐Werner Olfs 《植物养料与土壤学杂志》2007,170(2):210-218

A 90‐day laboratory incubation study was carried out using six contrasting subtropical soils (calcareous, peat, saline, noncalcareous, terrace, and acid sulfate) from Bangladesh. A control treatment without nitrogen (N) application was compared with treatments where urea, ammonium sulfate (AS), and ammonium nitrate (AN) were applied at a rate of 100 mg N (kg soil)^–1. To study the effect of N fertilizers on soil carbon (C) turnover, the CO₂‐C flux was determined at nine sampling dates during the incubation, and the total loss of soil carbon (TC) was calculated. Nitrogen turnover was characterized by measuring net nitrogen mineralization (NNM) and net nitrification (NN). Simple and stepwise multiple regressions were calculated between CO₂‐C flux, TC, NNM, and NN on the one hand and selected soil properties (organic C, total N, C : N ratio, CEC, pH, clay and sand content) on the other hand. In general, CO₂‐C fluxes were clearly higher during the first 2 weeks of the incubation compared to the later phases. Soils with high pH and/or indigenous C displayed the highest CO₂‐C flux. However, soils having low C levels (i.e., calcareous and terrace soils) displayed a large relative TC loss (up to 22.3%) and the added N–induced TC loss from these soils reached a maximum of 10.6%. Loss of TC differed depending on the N treatments (urea > AS > AN >> control). Significantly higher NNM was found in the acidic soils (terrace and acid sulfate). On average, NNM after urea application was higher than for AS and AN (80.3 vs. 71.9 and 70.9 N (kg soil)^–1, respectively). However, specific interactions between N‐fertilizer form and soil type have to be taken into consideration. High pH soils displayed larger NN (75.9–98.1 mg N (kg soil)^–1) than low pH soils. Averaged over the six soils, NN after application of urea and AS (83.3 and 82.2 mg N (kg soil)^–1, respectively) was significantly higher than after application of AN (60.6 mg N (kg soil)^–1). Significant relationships were found between total CO₂ flux and certain soil properties (organic C, total N, CEC, clay and sand content). The most important soil property for NNM as well as NN was soil pH, showing a correlation coefficient of –0.33** and 0.45***, respectively. The results indicate that application of urea to acidic soils and AS to high‐pH soils could be an effective measure to improve the availability of added N for crop uptake.  相似文献   

Long‐term effects of fertilization on some soil properties under rainfed soybean‐wheat cropping in the Indian Himalayas     

Ved Prakash  Ranjan Bhattacharyya  Govindan Selvakumar  Samaresh Kundu  Hari Shanker Gupta 《植物养料与土壤学杂志》2007,170(2):224-233

This study aims to examine the effects of long‐term fertilization and cropping on some chemical and microbiological properties of the soil in a 32 y old long‐term fertility experiment at Almora (Himalayan region, India) under rainfed soybean‐wheat rotation. Continuous annual application of recommended doses of chemical fertilizer and 10 Mg ha^–1 FYM on fresh‐weight basis (NPK + FYM) to soybean (Glycine max L.) sustained not only higher productivity of soybean and residual wheat (Triticum aestivum L.) crop, but also resulted in build‐up of total soil organic C (SOC), total soil N, P, and K. Concentration of SOC increased by 40% and 70% in the NPK + FYM–treated plots as compared to NPK (43.1 Mg C ha^–1) and unfertilized control plots (35.5 Mg C ha^–1), respectively. Average annual contribution of C input from soybean was 29% and that from wheat was 24% of the harvestable aboveground biomass yield. Annual gross C input and annual rate of total SOC enrichment from initial soil in the 0–15 cm layer were 4362 and 333 kg C ha^–1, respectively, for the plots under NPK + FYM. It was observed that the soils under the unfertilized control, NK and N + FYM treatments, suffered a net annual loss of 5.1, 5.2, and 15.8 kg P ha^–1, respectively, whereas the soils under NP, NPK, and NPK + FYM had net annual gains of 25.3, 18.8, and 16.4 kg P ha^–1, respectively. There was net negative K balance in all the treatments ranging from 6.9 kg ha^–1 y^–1 in NK to 82.4 kg ha^–1 y^–1 in N + FYM–treated plots. The application of NPK + FYM also recorded the highest levels of soil microbial‐biomass C, soil microbial‐biomass N, populations of viable and culturable soil microbes.  相似文献   

秸秆还田配施氮肥对稻田土壤活性碳氮动态变化的影响   总被引：3，自引：1，他引：2  

王士超  闫志浩  王瑾瑜  槐圣昌  武红亮  邢婷婷  叶洪龄  卢昌艾 《中国农业科学》2020,53(4):782-794

【目的】土壤微生物量碳氮和水溶性有机碳氮是土壤中最活跃的碳氮组分,是衡量土壤碳氮周转与养分有效性的重要指标。探讨秸秆配施氮肥、氮肥用量及基追比例对稻田土壤微生物量碳氮、水溶性有机碳氮、易氧化有机碳和速效氮的影响,明确秸秆还田条件下水稻生长季不同氮肥用量与基追比的土壤活性碳氮变化特征,为稻麦轮作区秸秆还田的氮肥管理提供理论依据。【方法】2012—2015年在湖北省荆门市田间试验中设置施氮量、秸秆配施氮肥和施氮时期3个大田试验。施氮量：不施氮（N0）,推荐施氮（165 kg·hm ^-2,N165）,习惯施氮（195 kg·hm ^-2,N195）;秸秆配施氮肥：秸秆移除（CK）,秸秆还田（移栽前将上季小麦秸秆全部还田,S）,秸秆还田+习惯施氮量（SN）,秸秆还田+推荐施氮量（SF）,秸秆还田+推荐施氮量+腐解菌剂（SM）;施氮时期：基施﹕拔节期﹕抽穗期氮肥施用比例为7﹕3﹕0（R1）,5﹕3﹕2（R2）,10﹕0﹕0（R3）。【结果】秸秆还田+习惯施氮量（SN）显著提高了水稻拔节期土壤微生物量碳（SMBC）含量,但是其成熟期水溶性有机碳含量（DOC）显著降低。秸秆还田+推荐施氮量（SF）显著提高了水稻拔节期土壤水溶性有机氮含量（DON）。腐解菌剂的施用显著降低了水稻成熟期DON含量,拔节期易氧化有机碳含量（ROC）也显著降低。秸秆还田下增加氮肥用量显著提高了水稻抽穗期和灌浆期土壤速效氮含量（AN）;推荐施氮处理（165 kg N·hm ^-2）的DON和AN含量显著升高;农民习惯施氮处理（195 kg N·hm ^-2）降低了DON和AN含量;增加追施氮肥比例对土壤SMBC和DOC含量无明显影响,但提高了水稻拔节期SMBN和ROC含量。【结论】施氮量及其基追比是影响秸秆还田下稻田土壤活性碳氮含量的主要因素,合理配施氮肥能提高土壤微生物量碳、速效氮及水溶性有机氮等活性碳氮组分含量,增加追肥比例也能提高水稻生育期内土壤活性碳氮含量。  相似文献   

不同有机肥对矿区复垦土壤磷素矿化特征研究   总被引：2，自引：0，他引：2  

吕鉴于  高文俊  郝鲜俊  张若扬  张博凯  薛玉晨 《灌溉排水学报》2020,(4):59-67

【目的】探究不同有机肥对采煤塌陷复垦土壤磷素的矿化特征。【方法】采用室内培养试验,以不施肥处理为空白处理(CK),研究了施用3种有机肥(鸡粪、猪粪、牛粪)对矿区复垦土壤速效磷的动态变化,并综合其矿化过程中的磷酸酶活性及磷转化强度,分析了不同有机肥对矿区复垦土壤磷生物有效性的影响。【结果】①在整个室内恒温培养过程中,各施肥处理的速效磷量均随培养时间延长呈下降趋势,不同培养时期速效磷量大致呈现出:鸡粪>猪粪≥牛粪>化肥>CK。培养结束时(105d),鸡粪、猪粪和牛粪处理较化肥处理显著提高了土壤速效磷量(18.56%~37.09%);鸡粪处理较猪粪和牛粪处理速效磷量显著提高了11.93%~15.62%,而猪粪和牛粪处理间差异不显著;②在整个室内恒温培养过程中,拟二阶动力学模型能较好地反映各施肥处理速效磷释放过程,其次为Elovich模型和幂函数模型,而粒内扩散模型拟合效果较差。③在整个培养时期施有机肥处理的磷酸酶活性显著高于化肥处理,提高幅度为39.14%~120.70%。④培养前期(0~14 d),猪粪处理与化肥处理对土壤有机磷转化强度影响较大,二者间差异不显著,且猪粪处理较牛粪、鸡粪处理能显著提高有机磷转化强度,分别提高了41.51%和86.52%;在培养中后期(42~105d)各施肥处理的有机磷转化强度差异均不显著。【结论】施用有机肥能促进矿区复垦土壤磷素矿化,其中鸡粪较猪粪和牛粪对提高土壤有效磷量作用更为明显。  相似文献   

山西省畜禽粪污土地承载力及粪尿替代化肥潜力分析   总被引：1，自引：0，他引：1  

郭彩霞  杨子森  马文奇  焦光月  张建杰 《农业环境科学学报》2020,39(7):1548-1557

为明确山西省畜牧业的发展规模,优化畜牧业发展的空间格局,进一步为山西省农牧业实现绿色发展提供科学依据。研究基于农牧生产系统养分平衡的方法,测算了山西省县域尺度的畜禽粪污土地承载力。结果表明,山西省的种植业与畜牧业发展规模在空间上存在一定的错位,种植业发达的地区主要分布在省域南部和中部的区县,而畜牧业发达的地区则分布在省域北部、中部和东南部的区县;山西省当前的畜牧业发展规模折合为2 371.77万猪当量,以粪尿氮作为约束指标,山西畜牧业可发展规模为5 976.01万猪当量;以粪尿磷(纯磷,下同)作为约束指标,山西畜牧业可发展规模为7 212.27万猪当量。综合粪尿氮磷承载力指数结果分析,超载区域主要分布在省域北部种植业欠发达的区县和省城太原周边的区县;全省粪尿氮、磷的有效供给量分别为18.28万t和3.15万t,可以分别有效替代氮、磷肥39.79%和33.21%。无论以粪尿氮或磷作为约束指标,山西畜牧业整体上仍有较大的发展空间,可适度增加畜禽养殖规模,但需要关注城市近郊区县的畜禽粪尿氮磷的环境排放和大中型养殖企业的点源污染问题。在畜禽粪尿养分资源管理策略上,则应考虑优化农牧业生产布局和区域间协同管理。  相似文献