黄土丘陵区撂荒群落演替序列种根系对氮素施肥方式和水平的形态响应

采用盆栽试验,研究了黄土丘陵区撂荒群落演替序列种(即,黄土丘陵区摞荒群落演替主要阶段的优势种)根系对氮素施肥方式和水平的形态响应,对了解我国氮沉降增加背景下的群落生态效应及人为施肥干扰促进植被恢复具有较好的理论和实践意义。测试并分析了6个演替序列种在不同施氮方式(匀质和异质施氮)和水平(高、低和无氮对照)条件下植株个体生物量指标(地上及地下生物量和根冠比)、根系形态指标(根长、直径、表面积、比根长和比表面积)的变化及其差异显著性;并且利用根钻法和单样本T检验比较了异质施氮方式下施氮斑块与不施氮斑块根系形态指标的差异。结果表明:1)6种演替序列种地上、地下生物量和根冠比存在种间固有差别,施氮方式和水平整体上对三者无显著影响;施氮方式和植物种类对根冠比存在显著交互作用,说明个别种的根冠比对施氮方式响应明显,其中猪毛蒿根冠比在异质施氮方式下显著高于匀质施氮。2)6种演替序列种根系塑形指标包括比根长、比表面积和直径存在种间差别,并且施氮水平对比根长影响显著,高、低施氮水平下比根长都显著低于不施氮对照。3)狗尾草和铁杆蒿分别在异质高氮和异质低氮条件下施氮斑块根系生物量密度显著高于未施氮斑块;猪毛蒿在异质高氮条件下施氮斑块发生了更多的伸长生长,其根长、根表面积、比根长和比表面积在施氮斑块中的密度显著高于未施氮斑块;猪毛蒿和狗尾草在异质高氮条件下,以及白羊草在异质低氮条件下,其根系直径在施氮斑块显著小于未施氮斑块。从根系形态变化敏感性和施氮对促进植物生长来看,演替过程中演替序列种对施氮响应的敏感性总体上呈降低趋势,前期种对施氮响应更敏感,从施氮获利也更多,因而恢复前期进行人为干扰促进植被恢复效果也会更好。     

施氮深度和水分胁迫对藜麦幼苗生理及产量的影响

为了探讨藜麦应对施肥深度和水分胁迫的响应,该文以藜麦(Chenopodium quinoa)为材料,在盆栽条件下,设置3种施氮处理[D1(控释尿素施在0～8 cm深度)、D2(控释尿素施在8～16 cm深度)、D3(控释尿素施在16～24 cm深度)]和3种水分处理[W1(正常供水)、W2(中度干旱)、W3(重度干旱)],分析施氮深度和水分胁迫对藜麦幼苗生理及产量的影响。结果表明:(1)相同水分条件下,随着施肥深度的增加,藜麦生长指标(株高、茎粗、叶面积、地上部生物量、主根长、根系表面积、根系体积)、生理指标 [超氧化物歧化酶(SOD)活性、过氧化物酶(POD)活性、过氧化氢酶(CAT)活性、可溶性糖含量、可溶性蛋白含量、叶绿素总量]和产量指标呈先升高后降低趋势。D2处理(适当的深施氮肥)均高于D1处理(浅层施氮)和D3处理(底层施氮)。(2)相同施氮深度条件下,随着干旱胁迫程度的增加,藜麦生长指标和产量指标呈逐渐降低的趋势,生理指标均呈先升高后降低的趋势。说明藜麦幼苗对水分需求明显,可通过增加抗氧化酶活性和渗透调节物质适应一定程度的干旱,生产实践中应注意苗期水分的供应,以促进生育后期产量的形成。综上可知,适宜的水氮管理(D2W1)可以促进藜麦的生长及生理特性,增强藜麦的抗旱能力,提高藜麦的产量。该研究结果为进一步研究藜麦的水肥管理、高产栽培提供参考。     

施氮对干旱胁迫下毛竹幼苗生物量和根系形态的影响

为探讨氮素添加对水分胁迫下毛竹幼苗地上生物量及地下根系形态的调控作用,选取1年生毛竹实生苗为材料,采用水分和施氮双因素完全随机区组设计,以田间持水量的80%～85%作为水分对照(CK)、50%～55%为中度干旱(MD)、30%～35%为重度干旱(HD)设置3个水分水平,氮处理分未施氮(N0,0 mg N·kg^-1)和施氮(N1,100 mg N·kg^-1)2个水平,通过盆栽试验,测定毛竹实生苗根系形态特征及各器官生物量。结果显示：施氮显著增加了同一水分下毛竹幼苗叶、根及整株生物量,其中,N1MD和N1HD分别较N0MD和N0HD地上生物量增加15.6%、11.9%,总生物量分别增加36.7%、25.0%(P<0.05);施氮降低了相同水分处理下毛竹的比根长、茎叶比,显著促进了中度和重度干旱下根冠比的增加(P<0.05);水分胁迫下,除根生物量比显著增加外,茎、叶生物量比均随氮素添加呈减小的趋势;施氮对毛竹幼苗根系形态特征(根长、根表面积、根体积)具有不同程度的促进作用;施氮对中度干旱下毛竹幼苗干物质积累的缓解作用比重度干旱大,但在...     

施氮量及底追比例对小麦产量、土壤硝态氮含量和氮平衡的影响

研究了高产麦田中施氮量和底追比例对冬小麦籽粒产量、土壤硝态氮含量和氮素平衡的影响。田间试验在山东省龙口市中村进行,试验区小麦各生育阶段的降雨量和零度以上的积温分别为:82.9mm,649.8℃(播种~冬前)、33.3mm,578.7℃(冬前~拔节)2、8mm,359℃(拔节~开花)、84.3mm,837.6℃(开花~成熟)。试验设3个施氮量:0kg.hm-2(CK)、168kg.hm-2(A)、240kg.hm-2(B);在施氮量168kg.hm-2和240kg.hm-2条件下分别设3个底追比例:1/2∶1/2(A1和B1)、1/3∶2/3(A2和B2)、0∶1(A3和B3)。结果表明:不同施氮处理之间植株氮积累量无显著差异;与不施氮处理相比,施氮可显著提高籽粒产量和蛋白质含量,施氮量为168kg.hm-2、底追比例为1/3∶2/3的处理A2与处理B2、B3差异不显著,但处理A2显著提高了氮肥利用率,降低了土壤残留量和氮素表观损失量;施氮量相同,适当增加追施氮肥的比例可显著提高籽粒产量、蛋白质含量和氮肥利用率。试验还表明,在拔节期,底施氮量为84kg.hm-2和120kg.hm-2的处理A1、B1,在80~100cm和100~160cm土层分别出现硝态氮的累积;而底施氮量为56kg.hm-2的处理A2,在0~200cm土层硝态氮含量和累积量与不施氮处理无显著差异。在成熟期,追施氮量大于160kg.hm-2的处理B3、A3和B2,硝态氮在120~180cm土层出现累积高峰,已下移到小麦根系可吸收范围之外,易于造成淋溶损失;而追氮量为112kg.hm-2的处理A2,在100~200cm土层硝态氮累积量与对照无显著差异。试验中,施氮量为168kg.hm-2底追比例为1/3∶2/3的处理A2的籽粒产量、蛋白质含量、地上部植株氮肥吸收利用率、氮肥农学利用率和籽粒氮肥吸收利用率均较高,100~200cm土层未出现硝态氮的明显累积,氮素表观损失量最少,为最佳氮肥运筹方式。     

水分胁迫和氮肥对花生根系形态发育及叶片生理活性的影响

以"花育22号"花生为试验材料,在中度干旱胁迫和充足灌水两个水分条件下,分别设置不施氮肥(N0)、中氮(N1,90 kg·hm-2)、高氮(N2,180 kg·hm-2)3个施氮水平,研究不同土壤水分和氮肥条件对花生叶片生理活性及根系形态发育特征的影响.结果表明:与不施氮肥处理相比,两个水分条件下中氮处理均显著增加花生产量,但对收获指数无显著影响.干旱胁迫条件下,中氮处理对总根系生物量和总根长无显著影响,但显著增加花生总根系表面积;中氮和高氮处理均显著增加20~40 cm土层内根长和根系表面积,且高氮处理显著增加40 cm以下土层内根系生物量和根系表面积;施用氮肥显著提高叶片过氧化氢酶(CAT)和过氧化物酶(POD)活性,而丙二醛(MDA)含量随施氮量的增加而降低.正常供水条件下,施用氮肥显著降低了花生根系表面积和40 cm以下土层内根系生物量、根长和根系表面积,中氮处理可提高叶片保护酶活性.相关性分析表明,20~40 cm土层内根长和叶片超氧化物歧化酶(SOD)、CAT、POD活性与产量呈显著相关.     

施氮和增温对降香黄檀幼苗生长发育和生理特征的影响

采用添加氮素模拟氮沉降和人工气候箱模拟增温的方法,设置了对照、施氮、增温以及增温 ×施氮交互作用4个处理,分析不同处理对降香黄檀(Dalbergia odorifera T.Chen)幼苗生长形态变化、生物量的积累、叶片和根系生理方面的影响.结果显示:与对照相比,增温、施氮以及增温 ×施氮交互作用均促进了降香黄檀幼苗的...     

氮磷肥配施对苦荞根系生理生态及产量的影响

以苦荞品种‘迪庆’为材料,在盆栽试验条件下,研究了氮(纯氮用量分别为0g/kg、0.1g/kg、0.2g/kg)、磷(P2O5用量分别为0.1g/kg和0.2g/kg)配施对苦荞根系生长、生理指标及其产量的影响,旨在为黄土高原苦荞高产优质栽培提供理论依据。结果表明:(1)在相同施磷量条件下,苦荞幼苗的株高、茎粗、茎叶干重、主根长、根表面积、根系体积、根系直径、根系干重以及壮苗指数等均随施氮量的增加而呈先升后降的趋势,但根冠比随施氮量的增加而呈先降后升的趋势;叶片叶绿素含量以及根系活力、酸性磷酸酶(Apase)活性、可溶性蛋白含量和植株氮积累量随施氮量的增加呈抛物线变化趋势,根系硝酸还原酶(NR)活性和植株氮含量随施氮量的增加而增加;而根系可溶性糖含量、超氧化物歧化酶(SOD)活性、过氧化物酶(POD)活性、丙二醛(MDA)含量和游离脯氨酸含量等指标均随施氮量的增加而呈先降后升的趋势,0.1g/kg施氮处理各指标均显著低于其他处理;成熟期单株粒重、百粒重随施氮量的增加呈先升后降的趋势,0.1g/kg施氮处理各指标均显著高于其他处理。(2)在相同施氮量条件下,随着施磷量的增加,苦荞根系酸性磷酸酶(Apase)活性、SOD活性、POD活性、MDA含量、可溶性糖含量、可溶性蛋白以及游离脯氨酸含量等指标均降低,其余各指标则呈增加趋势。(3)无论施磷量条件如何,0.1g/kg的施氮处理下苦荞产量最高,与其他施氮处理相比,在低磷和高磷处理下的增产幅度分别为7.04%~37.40%和14.73%~68.26%;在施氮量一定的情况下,高磷处理比低磷处理增产15.96%~42.00%。(4)在该试验条件下,适当的氮磷肥配施表现出了明显的正加和效应,但过量施肥也有可能导致增产幅度下降,中氮高磷(施纯N量0.1g/kg,施P2O5量0.2g/kg)配施效果最优。     

模拟降水变化和土壤施氮对浙江古田山5个树种幼苗生长和生物量的影响

为了探讨古田山地区5个树种—秃瓣杜英(Elaeocarpus glabripetalus)、枫香(Liquidambar formosana)、木荷(Schima superba)、青冈(Cyclobalanopsis glauca)和马尾松(Pinus massoniana)幼苗的生长和生物量及其分配对添加氮肥和减少降水的响应, 在野外设置了双因素氮肥(对照和施氮)和降水(自然降水(对照)和减少降水)控制试验, 氮肥的施入量为10 g·m^-2·a^-1 NH₄NO₃, 分别于每年5月初和7月初各施5 g·m^-2·a^-1, 减少降水处理是减少自然降水的30%。经过3个生长季的处理发现: 1)施氮显著促进了秃瓣杜英、枫香和木荷的苗高和基径的生长, 并且对秃瓣杜英和枫香的促进作用经过1个生长季的处理就表现出来, 而木荷在经过2个生长季后才表现出来; 2)施氮显著促进了秃瓣杜英、枫香和木荷的全株生物量以及各部分生物量的增长, 而只增加了马尾松的侧枝和叶片生物量以及青冈的侧枝生物量; 3) 2个生长季的施氮处理提高了秃瓣杜英和木荷的叶重比以及枫香和青冈的枝重比, 3个生长季的施氮处理促进了秃瓣杜英、枫香和木荷的茎重比以及青冈和马尾松的枝重比, 地上干物质分配比例的增加以地下干物质分配比例减小为代价, 施氮后显著降低了秃瓣杜英、枫香、木荷和青冈的根重比和根冠比; 4) 降水减少30%对各树种的生长均无显著影响。     

农田施氮对水质和氮素流失的影响

基于ISI Web of Science数据库,利用文献计量学方法分析了自1957年以来各国在农田氮流失领域的研究发展态势,综述了农田氮流失特征及氮流失防控措施。结果表明,目前各国对农田氮流失的研究主要集中在施氮对水体水质的污染和监测方法上,涉及的关键词主要有Groundwater、Water quality、Surface water、Nitrate pollution、Eutrophication、Contamination、Nonpoint source pollution、Lysimeter、Runoff、Subsurface drainage等。中国、美国和加拿大等农业大国的研究机构在这一领域的研究成果最多发文量最多的期刊主要分布在荷兰、美国和中国。文献分析表明,受降水、地形、土壤、施肥等诸多管理措施的影响,不同区域的农田氮流失量差别很大,中国各类农田的氮流失量(13.7—347 kg/hm~2)明显高于欧美国家(4—107 kg/hm~2)。我国单位面积化肥(357.3 kg/hm~2)和氮肥(165.1 kg/hm~2)施用量均远高于世界平均用量(87.5 kg/hm~2和52.9 kg/hm~2),当季氮肥利用率(17%)却明显低于世界平均水平(58%),表明氮肥施用过量且利用率过低是造成氮流失的关键因素。综合分析农田氮流失防控措施发现,从源头控制氮流失是最有效的措施,优化农艺管理措施和氮迁移过程拦截等分别可减少15%—92%、46%—77%的氮素流失,其中针对农田适宜施氮量的研究最多。然而,面对粮食生产需求与资源短缺、水体水质持续恶化的现状,未来的研究重点应从简单的表观平衡向整个农田生态系统的氮素循环过程转变,更为迫切的是加快探索以水质保护为目标的化肥氮施用阈值(造成环境污染的临界施氮量),并推广示范这些有效的氮流失防控措施。     

施氮和供水对混播和单播白羊草叶片叶绿素荧光特性的影响

为明确干旱条件下混播和施氮对白羊草〔Bothriochloa ischaemum(Linn.)Keng〕叶片叶绿素荧光参数的影响,采用盆栽法并设置不同混播比例〔白羊草与柳枝稷(Panicum virgatum Linn.)混播比例分别为8:0、6:2、4:4和2:6〕、施氮水平(即不施氮和1kg干土施01g纯氮)和供水条件(即正常供水和干旱胁迫6d后复水),对白羊草叶片叶绿素荧光参数的变化进行比较分析;在此基础上,采用一般线性模型分析这3个因素及其交互作用对白羊草叶绿素荧光参数的影响效应.结果显示:正常供水条件下,各处理组白羊草的最大光化学效率(Fv/Fm)、实际光化学效率(ΦPSⅡ)、表观光合电子传递速率(ETR)、光化学淬灭系数(qP)和非光化学淬灭系数(NPQ)均无明显变化.干旱及复水条件下,不施氮处理组白羊草的Fv/Fm值在干旱胁迫6 d(即土壤相对含水量最低)时降至最低值,并在复水2 d后恢复至与正常供水条件下相近的水平,而施氮处理组的Fv/Fm值则一直保持与正常供水条件下相近的水平;不论施氮与否,各处理组白羊草的ΦPSⅡ、ETR、qP和NPQ值基本上均表现为在干旱胁迫6 d时达到最高值,并在复水2 d后恢复至正常供水条件下各参数值的90%以上.总体上看,混播白羊草的qP和ETR值均高于单播白羊草,而其NPQ值则低于后者.统计分析结果表明:混播比例、施氮水平和供水条件3个因素间的交互作用对白羊草的ΦPSⅡ、qP和ETR值无显著影响,施氮水平对NPQ值的单独作用、施氮水平和混播比例的交互作用对Fv/Fm值以及施氮水平和供水条件的交互作用对ETR值也无显著影响,但这3个因素的单独作用及两两因素间的交互作用对白羊草其余叶绿素荧光参数均有显著或极显著影响.研究结果表明:一定程度的干旱胁迫有利于提高白羊草叶片PSⅡ反应中心的开放程度、光合电子传递速率和热耗散过剩光能的能力;在干旱胁迫条件下,施氮有助于白羊草叶片维持PSⅡ反应中心的活性和光化学效率;并且,与柳枝稷适度混播可改善白羊草叶片的光合性能,提高其种间竞争适应性.     

Available soil nitrogen in relation to fractions of soil nitrogen and other soil properties

The available N of 27 soils from England and Wales was assessed from the amounts of N taken up over a 6-month period by perennial ryegrass grown in pots under uniform environmental conditions. Relationships between availability and the distribution of soil N amongst various fractions were then examined using multiple regression. The relationship: available soil N (mg kg^–1 dry soil)=(N_min×0.672)+(N_inc×0.840)+(N_mom×0.227)–5.12 was found to account for 91% of the variance in available soil N, where N_min=mineral N, N_inc=N mineralized on incubation and N_mom=N in macro-organic matter. The N mineralized on incubation appeared to be derived largely from sources other than the macro-organic matter because these two fractions were poorly correlated. When availability was expressed in terms of available organic N as % of soil organic N (N_ao) the closest relationship with other soil characteristics was: N_ao=[N_inc×(1.395–0.0347×CN_mom]+[N_mom×0.1416], where CN_mom=CN ratio of the macro-organic matter. This relationship accounted for 81% of the variance in the availability of the soil organic N.The conclusion that the macro-organic matter may contribute substantially to the available N was confirmed by a subsidiary experiment in which the macro-organic fraction was separated from about 20 kg of a grassland soil. The uptake of N by ryegrass was then assessed on two subsamples of this soil, one without the macro-organic matter and the other with this fraction returned: uptake was appreciably increased by the macro-organic matter.     

Sources,fates, and impacts of nitrogen inputs to terrestrial ecosystems: review and synthesis

The relative importance of nitrogen inputs from atmospheric deposition and biological fixation is reviewed in a number of diverse, non-agricultural terrestrial ecosystems. Bulk precipitation inputs of N (l–l2 kg N ha^–1 yr^–1) are the same order of magnitude as, or frequently larger than, the usual range of inputs from nonsymbiotic fixation (< 1=" –=" 5=" kg=" n=">^–1 yr^–1), especially in areas influenced by industrial activity. Bulk precipitation measurements may underestimate total atmospheric deposition by 30–40% because they generally do not include all forms of wet and dry deposition. Symbiotic fixation generally ranges from 10–160 kg N ha^–1 yr^–1) in ecosystems where N-fixing species are present during early successional stages, and may exceed the range under unusual conditions.Rates of both symbiotic and nonsymbiotic fixation appear to be greater during early successional stages of forest development, where they have major impacts on nitrogen dynamics and ecosystem productivity. Fates and impacts of these nitrogen inputs are important considerations that are inadequately understood. These input processes are highly variable in space and time, and few sites have adequate comparative information on both nitrogen deposition and fixation.

A method to optimize N-application in relation to soil supply of N,and yield of potato

Mathematical models of crop growth can provide estimates of the potential yield of potato, and also the minimum, critical N-concentration required, [N_c], to attain that yield. Efficient use of nitrogen requires that the crop incorporates sufficient nitrogen to attain its potential yield and that excess uptake is avoided. Predictions of the rate of supply of nitrogen from the soil are imprecise and so it has been difficult to estimate accurately the required application of fertilizer-N. Our work has shown the feasibility of using the growing crop as a monitor of the rate of supply of N from the soil. Using a low initial application rate of N at planting and monitoring uptake rate, we can estimate the contribution from the soil, and couple that information with estimates of yield and the related [N_c] to give an estimate of the requirement for supplementary applied-N. The method can be seen, therefore, as a means to determine the size of a second or subsequent part of a split application of fertilizer. This approach avoids much of the uncertainty over the fate of applied nitrogen and should offer growers the double benefits of economic use of fertilizer and of minimizing leaching losses. Further, by tailoring applications of N-fertilizer to the crop's requirements the grower will be better able to ensure the quality considerations in his crop.     

Variation in rates of nitrogen fixation in termites: response to dietary nitrogen in the field and laboratory

Abstract. Termites contribute nitrogen to their habitat through the nitrogenase activity of their bacterial symbionts. Previous studies indicate that high levels of dietary nitrogen suppress nitrogen fixation in termites. We examined the effects of dietary nitrogen on fixation rates in termites in both field and laboratory experiments. Ten field cplonies of Reticulitermes were collected and assayed for nitrogenase activity in July 1993, October 1993, January 1994, and April 1994. The nitrogen content of the wood collected with each colony was determined. There was no correlation between termite nitrogen fixation rates and the amount of nitrogen in their food for any of the four collection periods. In laboratory experiments, nitrogen fixation rates decreased when termites were fed filter paper treated with 2% and 5% ammonium nitrate or a 5% mixture of the amino acids proline, tryptophan and leucine, compared to water-treated controls. By contrast, the nitrogenase activity of termites fed filter paper treated with 2% and 5% ammonium phosphate, a mixture of the amino acids histidine, serine and aspartic acid, or 2% and 5% urea did not differ from the controls. However, nitrogenase activity increased when termites were fed with 2% uric acid. No clear association exists between termite nitrogen fixation and the nitrogen content of their food.     

Nitrogen inputs to a marine embayment: the importance of groundwater

We examined the importance of nitrogen inputs from groundwater and runoff in a small coastal marine cove on Cape Cod, MA, USA. We evaluated groundwater inputs by three different methods: a water budget, assuming discharge equals recharge; direct measurements of discharge using bell jars; and a budget of water and salt at the mouth of the Cove over several tidal cycles. The lowest estimates were obtained by using a water budget and the highest estimates were obtained using a budget of water and salt at the Cove mouth. Overall there was more than a five fold difference in the freshwater inputs calculated by using these methods. Nitrogen in groundwater appears to be largely derived from on site septic systems. Average nitrate concentrations were highest in the region where building density was greatest. Nitrate in groundwater appeared to behave conservatively in sandy sediments where groundwater flow rates were high (> 11/m²/h), indicating that denitrification was not substantially reducing external nitrogen loading to the Cove. Nitrogen inputs from groundwater were approximately 300 mmol-N/m³/y of Cove water. Road runoff contributed an additional 60 mmol/m³/y. Total nitrogen inputs from groundwater and road runoff to this cove were similar in magnitude to river dominated estuaries in urbanized areas in the United States.     

Microbial biomass and nitrogen cycling responses to fertilization and litter removal in young northern hardwood forests

The influence of site fertility on soil microbial biomass and activity is not well understood but is likely to be complex because of interactions with plant responses to nutrient availability. We examined the effects of long-term (8 yr) fertilization and litter removal on forest floor microbial biomass and N and C transformations to test the hypothesis that higher soil resource availability stimulates microbial activity. Microbial biomass and respiration decreased by 20–30 % in response to fertilization. Microbial C averaged 3.8 mg C/g soil in fertilized, 5.8 mg C/g in control, and 5.5 mg C/g in litter removal plots. Microbial respiration was 200 µg CO₂-C g^–1 d^–1 in fertilized plots, compared to 270 µg CO₂-C g^–1 d^–1 in controls. Gross N mineralization and N immobilization did not differ among treatments, despite higher litter nutrient concentrations in fertilized plots and the removal of substantial quantities of C and N in litter removal plots. Net N mineralization was significantly reduced by fertilization. Gross nitrification and NO₃ ^– immobilization both were increased by fertilization. Nitrate thus became a more important part of microbial N cycling in fertilized plots even though NH₄ ⁺ availability was not stimulated by fertilization.Soil microorganisms did not mineralize more C or N in response to fertilization and higher litter quality; instead, results suggest a difference in the physiological status of microbial biomass in fertilized plots that influenced N transformations. Respiration quotients (qCO₂, respiration per unit biomass) were higher in fertilized plots (56 µg CO₂-C mg C^–1 d^–1) than control (48 µg CO₂-C mg C^–1 d ^–1) or litter removal (45 µg CO₂-C mg C^–1 d^–1), corresponding to higher microbial growth efficiency, higher proportions of gross mineralization immobilized, and lower net N mineralization in fertilized plots. While microbial biomass is an important labile nutrient pool, patterns of microbial growth and turnover were distinct from this pool and were more important to microbial function in nitrogen cycling.     

Free amino acid, ammonium and nitrate concentrations in soil solutions of a grazed coastal marsh in relation to plant growth

Soluble free amino acids, ammonium and nitrate ions as sources of nitrogen for plant growth were measured in soils of a coastal marsh grazed by snow geese in Manitoba, Canada. Amounts of nitrogen, primarily ammonium ions, increased in the latter half of the growing season and over winter, but fell to low values early in the growing season. Free amino acid concentrations relative to ammonium concentrations were highest during the period of rapid plant growth in early summer, especially in soils in the intertidal zone, where the median ratio of amino acid nitrogen to ammonium nitrogen was 0·36 and amino acid concentrations exceeded those of ammonium ions in 24% of samples. Amino acid profiles, which were dominated by alanine, proline and glutamic acid, were similar to goose faecal profiles. In a continuous flow hydroponic experiment conducted in the field, growth of the salt‐marsh grass, Puccinellia phryganodes, on glycine was similar to growth on ammonium ions at an equivalent concentration of nitrogen. When supplies of soil inorganic nitrogen are low, amino acids represent a potentially important source of nitrogen for the re‐growth of plants grazed by geese and amino acid uptake may be as high as 57% that of ammonium ions.     

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。