The dynamics of nitrous oxide emission from the use of mineral fertilizers in Russia

The intensity of nitrous oxide (N2O) emission was considered based on literature data on the single input of mineral N (nitrogen) fertilizers into different agricultural soil types in Russia. Ambient environmental factors exert a combined effect on the process of gaseous nitrogen formation from fertilizers applied. To reduce the uncertainty of estimates as much as possible, only experimental results obtained under conditions similar to natural were selected for the assessments. Mineral nitric fertilizers were applied to soil at a rate of 40 to 75 kg/ha and the N2O emissions were measured for approximately 140 days. Daily average emission values varied from 0.08 to 0.45% of fertilizer nitrogen. Correspondingly, 1.26 and 2.38% of fertilizer nitrogen were emitted as N2O from chernozems and soddy podzols. In 1990, the use of fertilizers in Russian agricultural practices for 53 Gg N2O-N, which equates to approximately 6.1% of global nitrous oxide emissions from nitric fertilizers. Later, the emission dropped because of a decrease in the input of nitric fertilizers to agricultural crops, and in 1998, it constituted just 20.5% of the 1990 level. In the period from 2008 to 2012, the nitrous oxide emission is expected to vary from 0.5 to 65.0 Gg N2O-N due to possible changes in national agricultural development. In the most likely scenario, the use of mineral fertilizers in Russia will account for approximately 34 to 40 Gg N2O-N emissions annually from 2008-2012.     

Use and misuse of nitrogen in agriculture: the German story

Nitrogen (N) fertilization in agriculture has been discussed controversially in Germany for almost two centuries. The agronomist Carl Sprengel, who published his theory on the mineral nutrition of plants in 1828, advocated the use of mineral N fertilizers. Chemist Justus von Liebig, on the other hand, vehemently denied around 1850 the need for N fertilization. Although it soon became evident that Sprengel was right and Liebig was wrong, not much synthetic N fertilizer was used in German agriculture until around 1915, when the Haber-Bosch technique enabled the commercial production of NH3. The use of N fertilizers since then has grown, especially since 1950. To increase agricultural productivity, German governments have promoted, directly and indirectly, the use of N in crop and in animal production. Unfortunately, it was overlooked that N surpluses in agriculture increased rapidly; around 1980 they amounted yearly to more than 100 kg ha(-1). The extensive use of N in agriculture is causing environmental damage and is contributing substantially to the external costs of present agriculture. The main N compounds that affect the environment are N2O, NH3, and NO3. These compounds are considered to contribute one third to the external costs of agriculture. Additionally, the high rate of human intake of animal proteins and lipids has adversely affected the health of the country's population. Fundamental corrections in German farm policy appear inevitable.     

有机类肥料对土壤养分含量的影响

绿色、可持续是我国发展现代农业的必然要求,肥料投入是关键之一。基于有机肥培肥土壤、生态友好的优势,发展和推广有机肥已经成为我国农业生产的一项基本国策。我国有机肥来源广泛、种类繁多,农业生产条件千差万别。本文分析了我国有机肥产品种类及标准现状、理化性质差异、碳氮矿化特性差异及影响因素,评述了施用有机肥对提高耕地基础地力的作用。因来源、制作工艺不同,不同有机肥的有机碳组分含量、全氮和活性氮含量、碳氮比等基本性质差异明显,这四者是影响有机肥碳氮矿化率、碳氮矿化量、碱解氮释放量等碳氮供应特性的主要内在因素;加之土壤环境等外界因素的影响,不同有机肥表现出不同的养分供应特性。总体上,有机肥一方面对提高土壤有机质含量,尤其是活性有机质含量和碳库管理指数效果明显,另一方面可增加土壤氮磷钾养分容量,减少作物生长消耗带来的土壤养分亏损,促进土壤质量良性发展。今后,应加强有机肥在耕地培肥中的应用,并加强有机肥肥效理论的基础研究和安全高效有机肥新产品的开发,促进有机肥资源的高效循环利用,使其成为重要的农业资源。     

Advances in NANI and NAPI accounting for the Baltic drainage basin: spatial and temporal trends and relationships to watershed TN and TP fluxes

In order to assess the progress toward eutrophication management goals, it is important to understand trends in land-based nutrient use. Here we present net anthropogenic nitrogen and phosphorus inputs (NANI and NAPI, respectively) for 2000 and 2010 for the Baltic Sea watershed. Overall, across the entire Baltic, between the 5-year periods centered on 2000 and 2010, NANI and NAPI decreased modestly by ?6 and ?4%, respectively, but with substantial regional variation, including major increases in the Gulf of Riga drainage basin (+19 and +58%, respectively) and decreases in the Danish Straits drainage basin (?25 and ?40% respectively). The changes were due primarily to changes in mineral fertilizer use. Mineral fertilizers dominated inputs, at 57% of both NANI and NAPI in 2000, increasing to 68 and 70%, respectively, by 2010. Net food and feed imports declined over that period, corresponding to increased crop production; either fewer imports of food and feedstocks were required to feed humans and livestock, or more of these commodities were exported. A strong linear relationship exists between regional net nutrient inputs and riverine nutrient fluxes for both periods. About 17% of NANI and 4.7% of NAPI were exported to the sea in 2000; these relationships did not significantly differ from those for 2010. Changes in NANI from 2000 to 2010 across basins were directly proportional rather than linearly related to changes in total N (TN) fluxes to the sea (i.e., no change in NANI suggests no change in TN flux). Similarly, for all basins except those draining to the Baltic Proper, changes in NAPI were proportional to changes in total P (TP) fluxes. The Danish Straits decreased most between 2000 and 2010, where NANI and NAPI declined by 25 and 40%, respectively, and corresponding fluxes of TN and TP declined 31 and 18%, respectively. For the Baltic Proper, NAPI was relatively unchanged between 2000 and 2010, while riverine TP fluxes decreased 25%, due possibly to lagged effects of fertilizer reduction resulting from socio-political changes in the early 1990s or improvements in sewage treatment capabilities. For most regions, further reductions in NANI and NAPI could be achieved by more efficient production and greater substitution of manure for imported mineral fertilizers.     

长期不同施肥方式对麦田杂草群落的影响

以太湖地区农业科学研究所31a的长期肥料定位试验田为材料,分别于2011—2012年小麦苗期、拔节期和收获期进行了杂草群落调查,研究杂草类型与密度的分布、杂草多样性指数的变化,并对杂草种群分布与土壤养分因子进行冗余分析。结果表明:小飞蓬、看麦娘、大巢菜、稻槎菜、通泉草是本地区小麦生长期的主要杂草类型;随着小麦的生长以及氮肥、有机肥的施入,杂草密度呈下降趋势;施入有机肥降低了麦季杂草的群落多样性指数,在小麦生长的不同时期均衡施肥的CNPK处理以及不施肥的C0处理的群落各项多样性指数能维持在一个较高的水平。RDA分析显示土壤氮含量以及有机质含量与第一排序轴相关性大,是对杂草分布影响最大的两个土壤养分因子。太湖地区稻麦两熟制条件下,长期有机无机肥料单一或配合投入可显著影响麦田杂草的群落组成,其中氮肥和有机肥的施入能显著降低杂草密度;土壤养分的差异影响田面杂草密度和优势种群,均衡施肥能降低优势杂草种群的优势地位,抑制其发生危害程度,提高农田生态系统的生产力及稳定性。     

长期施肥对黄土旱塬农田土壤有机磷组分及小麦产量的影响

研究长期施肥对黄土旱塬农田土壤有机磷组分及小麦产量的影响,可为提高磷素转化利用率及合理利用肥料提供理论支持。本研究依托长武旱塬农田生态系统长期(1984—2016年)定位试验站,选取不施肥(CK)、单施氮肥(N)、单施磷肥(P)、施氮磷肥(NP)、单施有机肥(M)、氮肥配施有机肥(MN)、磷肥配施有机肥(MP)、氮磷肥配施有机肥(MNP)8个处理,研究其对土壤有机磷组分、小麦产量和土壤性质的影响。结果表明: 长期施肥后土壤有机磷含量为244.7～429.1 mg·kg^-1,除N处理外,其余各处理有机磷含量比CK均显著增加了15.4%～47.9%。长期施用磷肥改变了黄土旱塬农田表层土壤(0～20 cm)各有机磷组分含量,MP、MNP处理显著提高了活性有机磷及中活性有机磷含量;N、P和NP处理显著降低了中稳性有机磷含量;N、P、NP、MN、MP、MNP处理均显著提高了高稳性有机磷含量。各处理土壤有机磷组分与总有机磷含量比值为:中活性有机磷>高稳性有机磷>活性有机磷>中稳性有机磷。长期施肥后,与CK相比,氮、磷肥配施,尤其是与有机肥配施,显著增加了小麦生物产量和籽粒产量。土壤指标中,有机质、速效磷和无机磷与小麦产量呈显著正相关。MP、M处理可以显著提高黄土旱塬黑垆土中的速效磷、总磷、总无机磷、活性有机磷和中活性有机磷含量,表明有机肥与磷肥配施可以提高该地区更容易被作物吸收的磷组分。总之,氮磷肥配施并配施有机肥可以提高该地区磷供给,对小麦增产有促进作用,对提高黄土旱塬地区土壤质量有重要意义。     

有机无机肥配施提高麦-稻轮作系统中水稻氮肥利用率的机制

采用盆栽试验,研究了有机无机肥配施对麦-稻轮作系统中水稻氮素累积动态和土壤氮素供应动态的影响,并从微生物学角度探讨了有机无机肥协同提高水稻氮肥利用率的机制.结果表明：有机无机肥配施处理的土壤微生物生物量碳、氮和矿质态氮在水稻分蘖期前低于化肥处理,而在抽穗期至灌浆期显著高于其他处理.土壤氮素供应动态与水稻吸收利用氮素规律吻合程度最高,促进了水稻产量、生物量和氮素累积量的增加,显著提高了水稻的氮肥利用率.其主要机制是有机无机肥配施促进了土壤微生物繁殖,使其在水稻生育前期固持了较多的矿质氮,在水稻生育中、后期这些氮素逐渐被释放以供水稻吸收利用,较好地满足了水稻各阶段生长发育对氮素养分的需求.     

土壤微生物生物量氮对不同腐熟度有机肥的响应及对土壤矿质氮的调控作用

为探究化肥配施不同腐熟度有机肥对土壤微生物生物量氮(MBN)的影响及土壤MBN调控土壤矿质氮的作用,将堆肥过程与土壤培养试验相结合,设置常规化肥对照(CK)、化肥+腐熟度为50%(种子发芽指数为50%,下同)的有机肥(CO1)、化肥+腐熟度为80%的有机肥(CO2)、化肥+腐熟度为100%的有机肥(CO3)共4个处理,测定土壤MBN、矿质氮(NH₄⁺-N、NO₃^--N)、净硝化速率、微生物生物量碳(MBC)、可溶性有机碳(DOC)、脲酶和蛋白酶,并揭示土壤MBN对矿质氮的调控作用。结果表明: 到培养结束时,与CK处理相比,有机肥处理(CO1、CO2、CO3)的土壤MBN、NH₄⁺-N含量显著提高50.1%～62.4%、109.9%～147.1%,土壤NO₃^--N、净硝化速率显著降低23.3%～46.8%、26.2%～51.5%,土壤MBC、DOC含量、脲酶和蛋白酶活性分别显著提高33.8%～69.6%、7.4%～20.8%、11.2%～69.0%、9.4%～25.1%,且CO2、CO3的变化幅度均显著高于CO1。冗余分析和结构方程模型显示,较高腐熟度有机肥(腐熟度≥80%)对MBC、MBN、NH₄⁺-N含量、脲酶和蛋白酶活性具有正向调控作用,对土壤净硝化速率具有负向调控作用。化肥配施较高腐熟度有机肥可以明显增加土壤MBN,提升脲酶、蛋白酶活性,增加NH₄⁺-N含量,降低土壤净硝化速率。因此,在实际应用中,建议采用腐熟度为80%的有机肥与化肥配施,减少有机肥生产成本及时间,实现有机固体废弃物的资源化利用。     

The influence of mineral fertilizer combined with a nitrification inhibitor on microbial populations and activities in calcareous Uzbekistanian soil under cotton cultivation

Application of fertilizers combined with nitrification inhibitors affects soil microbial biomass and activity. The objective of this research was to determine the effects of fertilizer application combined with the nitrification inhibitor potassium oxalate (PO) on soil microbial population and activities in nitrogen-poor soil under cotton cultivation in Uzbekistan. Fertilizer treatments were N as urea, P as ammophos, and K as potassium chloride. The nitrification inhibitor PO was added to urea and ammophos at the rate of 2%. Three treatments--N200 P140 K60 (T1), N200 PO P140 K60 (T2), and N200 P140 PO K60 (T3) mg kg(-1) soil--were applied for this study. The control (C) was without fertilizer and PO. The populations of oligotrophic bacteria, ammonifying bacteria, nitrifying bacteria, denitrifying bacteria, mineral assimilating bacteria, oligonitrophilic bacteria, and bacteria group Azotobacter were determined by the most probable number method. The treatments T2 and T3 increased the number of oligonitrophilic bacteria and utilization mineral forms of nitrogen on the background of reducing number of ammonifying bacteria. T2 and T3 also decreased the number of nitrifying bacteria, denitrifying bacteria, and net nitrification. In conclusion, our experiments showed that PO combined with mineral fertilizer is one of the most promising compounds for inhibiting nitrification rate, which was reflected in the increased availability and efficiency of fertilizer nitrogen to the cotton plants. PO combined with mineral fertilizer has no negative effects on nitrogen-fixing bacteria Azotobacter and oligo-nitrophilic bacteria.     

The nitrogen fertilization of spring barley

Summary From 1971 to 1979 field trials with increasing rates of fertilizer nitrogen on spring barley with sugar beet as the preceding crop were conducted on a farm on sandy loam in the south western part of The Netherlands. Prior to sowing and fertilizing soil samples were taken and analysed for mineral nitrogen (N_min). The average yield increase through application of fertilizer nitrogen was only 750 kg of grain per ha per year, the maximum yield being about 5 tonnes per ha. In the case of a fixed rate of fertilizer nitrogen per annum it can be derived from the response curves that 60 kg of N would have given the smallest average yield deficit (170 kg grain per ha) in comparison with maximum yields. With an N-advisory system based on soil analysis the average yield deficit would be at a minimum (163 kg of grain per ha) with a value for mineral soil nitrogen+fertilizer nitrogen totalling 120 kg N per ha.No relationship was found between optimum rate of fertilizer nitrogen and the amount of mineral soil nitrogen at the end of the winter. This was ascribed to the relatively small variation in mineral soil nitrogen and the weak response of the crop to fertilizer nitrogen.Promising results from nitrogen fertilizing systems based on soil analysis can be expected from more responsive crops like winter wheat, sugar beets and potatoes.With the average yield deficit compared with maximum yield as a characteristic, the usefulness of any N-advisory system can be compared, taking a fixed rate of nitrogen system as a standard.Seconded by the Agricultural Bureau of the Netherlands Fertilizer Industry (LBNM).     

有机肥替代部分化肥对水稻光合速率、氮素利用率和产量的影响

农业生产中合理施用有机肥对实现化肥零增长、提高土壤肥力和保证粮食稳产高产至关重要.本试验在辽宁省沈阳市稻田以'沈农9816'为供试材料,设置7种不同处理,分别为不施氮肥(CK)、低氮150 kg ? hm-2(LN)、中氮240 kg ? hm-2(MN)、高氮330 kg·hm-2(HN)、中氮有机肥替代10％(OM...     

Revisiting the agronomic benefits of manure: a correct assessment and exploitation of its fertilizer value spares the environment

The ongoing disintegration of agriculture into specialized farms, specialized regions and even specialized countries, has disrupted local nutrient cycles. This process is promoted and sustained by the use of mineral fertilizers. Ample availability of mineral fertilizers has changed farmers' perception and appreciation of manure. By now, manure is looked upon as 'waste' in some regions. It is a contradiction in terms, however, to regard biological by-products as 'waste'. Apart from this cultural aspect, economical and environmental considerations per se, justify a rehabilitation of manure. First of all a correct assessment of the fertilizer value is required. The present paper explains how to determine the nitrogen fertilizer value (NFV) of manures in a unbiased manner. Subsequently, recommendations are made on how to exploit the potential NFV as good as possible. Undeniably, it is easier to manage mineral fertilizers than manure. However, when proper attention is given to the composition of manure and decisions on rates, timing and placement are made correspondingly, the NFV can be enhanced. This should lead to a drastic reduction of mineral fertilizer use, nutrient surpluses and environmental pollution. Under such conditions, 'manure', 'precision farming' and 'environment' can become reconciled again.     

长期施肥条件下黄土高原黑垆土作物产量与土壤碳氮的关系

通过设置在黄土高原黑垆土区的长期定位试验系统,研究了长期施肥条件下作物产量与土壤碳氮的互馈关系.试验设不施肥(CK)、单施氮肥(N)、氮磷配施(NP)、秸秆与氮磷配施(SNP)、施有机肥(M)和有机肥与氮磷配施(MNP)6个处理.结果表明: 与对照相比,长期平衡施用化肥、单施有机肥、化肥与有机肥配合施用和秸秆还田配施化肥显著增加了作物产量及其稳定性, NP、SNP、M、MNP处理玉米和小麦产量分别增加92%、97%、93%、141%和147%、164%、139%、214%.NP处理玉米和小麦年均产量与当地常规施肥作物产量相当且稳定,小麦-玉米轮作体系施肥量为N 90 kg·hm^-2、P₂O₅ 75 kg·hm^-2能够满足作物需要.秸秆还田与隔年施磷相配合的SNP处理与NP处理作物产量相似,且可减少磷肥施用量50%.平衡施用化肥、有机肥、化肥与有机肥配施和秸秆还田配施化肥均可显著增加土壤有机碳含量,而施用化肥对土壤全氮含量影响不明显,综合所有处理,土壤有机碳和全氮含量呈显著正相关.不同处理土壤有机碳固存率在15%～41%.SNP处理土壤有机碳累积投入量增加1 t·hm^-2,土壤有机碳含量增加0.06 g·kg^-1,而CK、N、NP、M和MNP处理的增幅在0.12～0.15 g·kg^-1.玉米和小麦产量都与土壤全氮含量呈显著正相关,玉米产量随土壤有机碳含量的增加而增加,但小麦产量随土壤有机碳含量的增加先快速增加后趋于平稳,拐点出现在6.8 g·kg^-1.长期平衡施用化肥、有机肥、有机肥与化肥配合施用及秸秆还田配施化肥可显著增加黄土高原黑垆土土壤有机碳和全氮含量、作物产量和根茬还田量,根茬还田量的增加又进一步增加了土壤有机碳和全氮含量,形成了相互促进的互馈关系.     

Best management practices for minimizing nitrate leaching from container-grown nurseries

Containerized plant production represents an extremely intensive agricultural practice; 40,000 to 300,000 containers may occupy one acre of surface area to which a large amount of chemical fertilizer is applied. Currently, recommended fertilizer application rates for the production of containerized nursery ornamental plants are in excess of plant requirements, and up to 50% of the applied fertilizers may run off or be leached from containers. Among the nutrients leached or allowed to runoff, nitrogen (N) is the most abundant and is of major concern as the source of ground and surface water pollution. In this report, current N fertilizer application rates for different container-grown nursery ornamental plants, the amount of nitrate leaching or runoff from containers, and the potential for nitrate contamination of ground and surface water are discussed. In contrast, our best N management practices include: (1) applying fertilizers based on plant species need; (2) improving potting medium's nutrient holding capacity using obscure mineral additives; (3) using controlled-release fertilizers; and (4) implementing zero runoff irrigation or fertigation delivery systems that significantly reduce nitrate leaching or runoff in containerized plant production and encourage dramatic changes in N management.     

氮肥种类及运筹技术调控土壤氮素损失的研究进展

氮肥的不合理施用导致氮肥利用率低下,大量氮素通过径流、淋溶、氨挥发、硝化-反硝化作用等途径损失到环境中,从而对水体、大气造成污染,带来严重的环境问题,影响人类健康.施氮量、施肥时间和方式,以及肥料种类对氮素流失量的影响显著.土壤氮素浓度过饱和是导致氮素大量流失的最根本原因,充分利用环境供氮量,减少化学氮肥施用量,采用深施等技术,以及配合施用有机肥,可以有效降低氮素的损失,提高氮素利用率.在开发应用新型高效氮肥和强化氮肥高效管理技术研究的同时,加强环境氮素的监测和利用力度,是实现减氮增效的有力手段.     

施肥对巢湖流域稻季氨挥发损失的影响

采用通气法对巢湖流域稻季土壤氨挥发原位监测,研究了不同施肥量及秸秆还田处理对稻季氨挥发的影响。结果表明,氨挥发峰值发生在施肥后的第1-3 天,氨挥发损失主要集中于施肥后的1周。2010年整个稻季氨挥发净损失量为7.22-14.20 kg/hm²,占氮肥施用量的4.59%-6.64%,基肥期是主要的氨挥发时期,约占总氨挥发量的60%,穗肥期氨挥发总损失量最小。常规施肥处理氨挥发总损失量最大,与常规施肥相比,优化施肥、减量化施肥均能减少稻田土壤氨挥发损失1%-2%,氮磷肥减量同时秸秆还田处理氨挥发量最小,其总氨挥发量占常规处理的54%。施肥后的1-2d内田面水中的NH₄⁺-N浓度达到最大值,且各施肥处理的氨挥发量与同期田面水中的NH₄⁺-N浓度呈线性正相关。结合经济效益和环境效应分析发现,秸秆还田处理可减少氨挥发损失,同时获得较高的经济效益,适宜在巢湖流域水稻季推广。     

有机无机肥分次配施对嘎啦苹果生长、15N-尿素吸收利用及损失的影响

以15年生嘎啦苹果/平邑甜茶为试材,采用¹⁵N同位素示踪技术,研究有机无机肥分次配施对嘎啦苹果/平邑甜茶生长、¹⁵N-尿素吸收利用及损失的影响.结果表明: 与不施有机肥相比,有机无机肥配施显著提高了植株根冠比、叶绿素含量、单株叶片总氮量和单果质量,且有机无机肥分次配施的效果要优于有机无机肥一次性配施.有机无机肥配施提高了各器官对氮的吸收征调能力(Ndff值),其中有机无机肥分次配施的效果更显著;而不同施肥处理各器官的Ndff值均表现为果实最高,其次是叶片、一年生枝、细根、粗根和多年生枝,中心干最低.有机无机肥分次配施植株总氮量和¹⁵N肥料利用率分别为395.39 g和28.4%,显著高于有机无机肥一次性配施处理(342.77 g和21.1%)和不施有机肥处理(296.41 g和14.6%),而¹⁵N损失率为51.3%,显著低于有机无机肥一次性配施处理(57.5%)和不施有机肥处理(60.6%).     

有机无机肥分次配施对嘎啦苹果生长、15N-尿素吸收利用及损失的影响

以15年生嘎啦苹果/平邑甜茶为试材,采用¹⁵N同位素示踪技术,研究有机无机肥分次配施对嘎啦苹果/平邑甜茶生长、¹⁵N-尿素吸收利用及损失的影响.结果表明: 与不施有机肥相比,有机无机肥配施显著提高了植株根冠比、叶绿素含量、单株叶片总氮量和单果质量,且有机无机肥分次配施的效果要优于有机无机肥一次性配施.有机无机肥配施提高了各器官对氮的吸收征调能力(Ndff值),其中有机无机肥分次配施的效果更显著;而不同施肥处理各器官的Ndff值均表现为果实最高,其次是叶片、一年生枝、细根、粗根和多年生枝,中心干最低.有机无机肥分次配施植株总氮量和¹⁵N肥料利用率分别为395.39 g和28.4%,显著高于有机无机肥一次性配施处理(342.77 g和21.1%)和不施有机肥处理(296.41 g和14.6%),而¹⁵N损失率为51.3%,显著低于有机无机肥一次性配施处理(57.5%)和不施有机肥处理(60.6%).     

贵州黄壤区辣椒干物质、氮素积累与分配及氮素利用对新型肥料的响应

为探索贵州黄壤区施用新型肥料对辣椒种植的增产效应,通过盆栽试验研究了保水型(BSX)、稳定性(WDX)、包膜型(BMX)缓释肥和长效氮肥(CXDF)4种新型肥料对‘博辣5号’辣椒的干物质、氮素积累与分配,以及氮素利用效率的影响.结果表明: 施用新型肥料可以明显影响辣椒干物质和氮素的积累与分配,辣椒氮素积累快速增长开始时间和结束时间较干物质分别提前17~26 d和28~45 d,且氮素积累快速增长持续期也较干物质缩短7~23 d,表明氮素积累的发生时间要先于干物质积累;与普通复合肥(FHF)处理相比,新型肥料处理的干物质和氮素积累均出现明显滞后,以BMX处理的滞后时间最长,但是WDX处理的快速增长持续期较短且最大积累速率最高,说明稳定性缓释肥可实现养分短时间内的高效利用;BSX和BMX处理的花后干物质和氮素积累量占总干物质和总氮的比例分别为62.9%和20.1%、73.3%和20.5%,而WDX处理则分别为59.3%和11.6%,说明保水型和包膜型缓释肥相对有利于辣椒花后干物质积累和氮素同化,而稳定性缓释肥则更有利于花前干物质和养分积累;与FHF处理相比,施用新型肥料(保水型、稳定性和包膜型缓释肥)可显著提高辣椒的氮素利用效率,以稳定性缓释肥的氮肥偏生产力、氮肥农学效率和氮肥表观利用率最高,分别为66.74 kg·kg^-1、44.28 kg·kg^-1和54.6%.新型肥料适用于贵州辣椒种植栽培,以稳定性缓释肥的施用效果最佳.     

Changa in the structure and activity of a soil microbial community caused by inorganic nitrogen fertilization

The changes in the structure and activity of a soil microbial community caused by addition of moderate and high rates of the mineral nitrogen fertilizer (KNO₃) were studied in a laboratory incubation experiment. The structure of the microbial community was evaluated from the phospholipid fatty acid (PLFA) profile; specific growth rate of the microorganisms was determined by the method of the kinetics of substrate-induced respiration; the total pool of microbial carbon was estimated by the fumigation-extraction method. The amounts of nitrogen fertilizer applied in three treatments of the experiment were 0 (control), 100, and 2000 ??g N/g soil. Even in the absence of additional sources of organic carbon, a considerable portion of the added ¹⁵N (up to 74%) was immobilized. No significant increase in the amount of microbial carbon was observed during incubation. The specific growth rate of the microbial community in soil supplemented with glucose decreased twofold after addition of 2000 ??g N/g soil. In this treatment, the ratio of cyclic fatty acids to their monoenoic precursors also increased, indicating the adaptation of microbial cells to extremely high amounts of nitrogen fertilizer. Moreover, considerable changes in the structure of the soil microbial community, such as an increase in the ratio of fungalto bacterial markers and a decrease in the ratio between PLFA of gram-positive and gram-negative bacteria, were observed in the treatment with addition of 2000 ??g N/g soil. Our data clearly indicate that mineral nitrogen fertilization of soil under carbon limitation has a pronounced impact on the structure and activity of soil microbial communities.