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1.
四种温带森林土壤氮矿化与硝化时空格局 总被引:11,自引:0,他引:11
利用PVC管原位培养连续取样法测定了东北地区4种具有代表性的森林生态系统(硬阔叶林、蒙古栎林、红松林、落叶松林)土壤氮素矿化、硝化的时间动态及氮矿化的空间分布格局.结果表明:4种森林土壤氮素矿化存在明显的时空变异.蒙古栎和红松林土壤在6月份表现出强烈的氮矿化和硝化作用,而硬阔叶林及落叶松林7月份氮素矿化强烈.4种森林生态系统上层土壤的氮净矿(硝)化率显著高于下层土壤.4种林型土壤的硝化过程在氮矿化过程中占有重要地位,其NO-3-N在无机氮中的比例分别为:79.9%~91.1%(硬阔叶林)、50.7%~80.5%(蒙古栎林)、54.1%~92.0%(红松林)、63.7%~86.5%(落叶松林).生态系统构成决定了土壤氮素的矿化能力.阔叶林和针阔混交林生态系统矿化率大于纯针叶林生态系统.硬阔叶林、红松林、蒙古栎林、落叶松林的平均净矿化率分别为:(0.58±0.01) mg · kg-1 · d-1、(0.47±0.19) mg · kg-1 · d-1、(0.39±0.11) mg · kg-1 · d-1和(0.23±0.06) mg · kg-1 · d-1.4种林型氮素矿化作用与地下5 cm温度呈正相关,并受土壤表层 (0~10 cm)水分显著影响.土壤微生物量氮与土壤氮矿化呈显著正相关. 相似文献
2.
宁南山区典型植物根际与非根际土壤碳、氮形态 总被引:2,自引:0,他引:2
以宁南山区典型植物冰草、冷蒿、长芒草、百里香和铁杆蒿为对象,研究不同植物根际土壤和非根际土壤碳、氮形态的变化.结果表明:5种植物对根际土壤和非根际土壤碳、氮含量的影响不同.其中,铁杆蒿的根际土壤碳含量最高,总有机碳、轻组有机碳和重组有机碳含量分别为22.94、1.95和20.88g·kg-1,长芒草的根际土壤氮含量最高,总氮、可矿化氮和速效氮含量分别为2.05g·kg-1、23.73mg·kg-1和11.99mg·kg-1.冷蒿的根际土壤中活性有机碳/总有机碳、可矿化氮/总氮最高,有利于土壤中碳素和氮素向活性态转变.轻组有机碳、可矿化氮可作为植物生境改变的敏感指标.5种植物根际土壤各形态碳、氮含量总体上高于非根际土壤. 相似文献
3.
武夷山不同海拔典型植被带土壤酶活性特征 总被引:10,自引:0,他引:10
在武夷山自然保护区不同海拔4个典型植被带(常绿阔叶林、针叶林、亚高山矮林以及高山草甸)采集土壤样品,分析了脲酶、蔗糖酶、酸性磷酸酶和过氧化氢酶4种主要土壤酶活性的变化.结果表明:除磷酸酶外,武夷山不同海拔植被带土壤酶活性没有显著的季节差异,磷酸酶活性秋季显著高于其他季节;不同海拔土壤酶活性差异显著,海拔与季节对土壤酶活性无交互影响;土壤酶活性随海拔升高总体上呈上升趋势,高海拔草甸的土壤酶活性显著高于低海拔林地土壤;土壤酶活性具有明显的垂直分层分布,土层越深酶活性越低;4个植被带土壤脲酶活性为1.28 ~3.87 mg·g-1·24h-1,高山草甸>常绿阔叶林>亚高山矮林>针叶林;蔗糖酶活性为36.18 ~244.08 mg·g-1·24 h-1,高山草甸>针叶林>常绿阔叶林>亚高山矮林;磷酸酶活性和过氧化氢酶活性分别为0.18~0.62 mg·g-1 ·2 h-1和1.78 ~1.98 ml·g-1·20 min-1,高山草甸>针叶林>亚高山矮林>常绿阔叶林;土壤酶活性与土壤总有机碳、全氮显著正相关;与土壤温度、湿度、pH相关性比较复杂. 相似文献
4.
大气氮沉降对阔叶林红壤淋溶水化学模拟研究 总被引:7,自引:0,他引:7
在氮饱和的森林生态系统中,氮沉降的增加将导致NO3-淋溶的增加及土壤酸度的提高,从而影响土壤质量及林业的可持续发展。然而,大气氮沉降对我国南方红壤地区森林生态系统中土壤的影响研究还很少,尤其是氮沉降引起的土壤淋溶液化学组成方面。研究中,以中国科学院红壤生态实验站林草生态试验区阔叶林红壤为对象,在恒温(20℃)条件下,通过土壤淋洗柱(直径10cm、高60cm)进行了8个月间隙性淋溶试验,来模拟研究不同氮输入量(0、7.8、26mg月-1.柱-1和52mg月-1柱-1)对阔叶林红壤NO3-、NH4 、SO42-、H 和土壤盐基离子(Ca2 、Mg2 、K 和Na )的淋溶和土壤酸度的影响。结果表明,随氮输入量增加,淋溶液中NO3-、EC、H 和总盐基离子逐渐增加,但淋溶液中无NH4 。不同氮处理时,土壤有机氮总表观矿化量分别为189.6、263.9、372.8mg月-1.柱-1与554.2mg柱-1,氮输入明显促进了土壤有机氮的矿化,且土壤有机氮的表观矿化量与氮输入量间呈正线性相关(R2=0.997**)。无氮(0mg月-1柱-1)、低氮(7.8mg月-1柱-1)、中氮(26mg月-1柱-1)和高氮(52mg月-1柱-1)输入处理下,土壤交换态盐基淋溶总量分别占土壤交换性盐基总量的13.6、18.4、27.7%和48.1%。不同的盐基离子对氮输入的反应不同,Ca2 和Mg2 淋溶量随氮输入量的增加而增加,对Na 和K 则无明显影响。土壤交换态离子中随淋洗液输出最多的为Ca2 (无氮、低氮、中氮和高氮输入处理的土壤交换态输出量占土壤交换态的比例分别为22.6、31.4、46.7%和82.5%),其次为Na (无氮、低氮、中氮和高氮输入处理的土壤交换态输出量占土壤交换态的比例分别为16.0、10.7、17.6%和26.3%),最少的为Mg2 (无氮、低氮、中氮和高氮输入处理的土壤交换态输出量占土壤交换态的比例分别为5.0、6.9、11.1%和16.9%),几乎没有土壤交换性K 输出。与对照相比,有氮处理后土壤中硫酸根离子的淋失量明显减少(p<0.05)。表层土壤pH值随氮输入量的增加而显著下降,各处理间差异极显著(p<0.01)。可见,大气氮沉降的增加将加速阔叶林红壤的养分淋失和土壤酸化的程度。 相似文献
5.
浙江天童地区常绿阔叶林退化对土壤养分库和碳库的影响 总被引:3,自引:0,他引:3
为了解常绿阔叶林退化对土壤碳库和养分库的影响,采用空间代替时间的研究方法,以常绿阔叶林顶级群落为参照,选择了次生常绿阔叶幼年林、次生针阔混交林、次生针叶林、灌丛和灌草丛代表不同的退化类型,分别对其土壤氮磷养分库、碳库进行了调查和分析。结果表明:土壤氮库贮量从大到小依次为,成熟常绿阔叶林、次生常绿阔叶幼年林、灌丛、次生针叶林、灌草丛和次生针阔混交林;土壤总磷含量也是在成熟林最高,次生针阔混交林和次生针叶林的总磷含量显著高于次生常绿阔叶幼年林和灌丛;土壤有机碳含量从高到低依次为:成熟常绿阔叶林,次生针叶林、次生常绿阔叶幼年林、灌丛、灌草丛和次生针阔混交林;土壤铵态氮在成熟林、灌丛和灌草丛的库容量最大,其次分别为次生幼年常绿阔叶林、次生针阔混交林,最小的为次生针叶林;硝态氮则在灌草丛的库容量最大,其次分别为次生针叶林、次生针阔混交林和成熟林针叶林,最小的为次生常绿阔叶幼年林和灌丛。统计显示,常绿阔叶林退化不仅导致土壤有机碳库含量的显著下降,也使得土壤氮磷养分库含量显著下降。可以认为,砍伐导致的大量生物量输出和森林管理措施的影响,植物种类组成的改变,土壤物理性质的改变以及养分和有机碳的主要生物化学转化环节发生改变是导致此类变化的主要因素,常绿阔叶林顶极群落土壤是该地区土壤的最大养分库和碳库。 相似文献
6.
控释尿素减施对双季稻田氮素渗漏淋失的影响 总被引:5,自引:0,他引:5
大量施用氮肥引起的土壤氮素淋失是稻田氮素损失的一个重要途径.为探究自然降雨过程中典型双季稻田氮渗漏淋失特点,采用田间渗漏池法,通过大田小区试验,研究控释尿素减施对稻田土壤60 cm深处渗漏水中氮淋失和水稻产量的影响.结果表明: 施肥初期出现氮渗漏淋失峰值,这是防控的关键时期;双季稻生长季控释尿素减氮20%(0.8CRU)和减氮30%(0.7CRU)处理全氮淋失量分别为42.3和37.7 kg·hm-2,均显著低于常规尿素(CU)处理(53.9 kg·hm-2),且0.7CRU处理显著低于等氮量控释尿素(1.0CRU)处理(51.3 kg·hm-2);各施氮处理全氮渗漏淋失率为11.9%~13.5%,处理间差异不显著.0.8CRU和0.7CRU处理较CU处理明显提高了水稻产量和氮肥吸收利用率,显著增加了氮收获指数.总之,控释尿素减氮 20%~30%能保证水稻产量和防控稻田氮渗漏淋失. 相似文献
7.
三峡库区不同植被类型土壤养分特征 总被引:24,自引:6,他引:18
通过三峡库区8个植被类型370个样地的群落调查和土壤分析,研究了不同植被类型、土壤类型、海拔对表层土壤有机质及全氮、速效磷、速效钾含量的影响.结果表明:(1)三峡库区不同植被类型土壤有机质、全氮平均含量规律为阔叶林>竹林>针叶林>灌丛>草丛,森林土壤有机质及全氮平均含量丰富;速效磷平均含量表现为草丛>落叶阔叶林>灌丛>暖性针叶林>常绿落叶阔叶混交林>温性针叶林>竹林>常绿阔叶林,草丛与其他植被类型差异显著;速效钾平均含量表现为常绿落叶阔叶混交林>落叶阔叶林>灌丛>针叶林>竹林>草丛>常绿阔叶林,竹林、草丛、常绿阔叶林与常绿落叶阔叶混交林、落叶阔叶林、灌丛、针叶林差异显著.(2)不同土壤类型养分含量差异显著,黄棕壤中有机质、全氮含量高,分别为6.83%、0.44%,紫色土中速效磷含量高,达到54.24mg/kg.(3)随海拔升高,有机质、全氮含量呈明显增加趋势,速效磷、速效钾含量变化趋势不明显. 相似文献
8.
土壤pH对东南景天修复镉和锌污染土壤的影响 总被引:1,自引:0,他引:1
《生态学杂志》2014,(11)
采用盆栽方法研究重金属(Zn、Cd)2种污染水平(T1处理:Zn 1200 mg·kg-1+Cd 20 mg·kg-1;T2处理:Zn 300 mg·kg-1+Cd 2.0 mg·kg-1)、4个p H水平(4.0、5.5、7.0和8.5)下,土壤Zn、Cd有效态的变化、东南景天吸收和积累特征以及植物对土壤中Zn、Cd的去除效果。结果表明,随着p H的降低,土壤Zn、Cd的有效态含量显著增大,东南景天吸收和积累土壤Zn、Cd的效率显著提高。T1处理时东南景天生物量在p H 5.5时最大,但与其他p H处理的差异并不显著;Zn、Cd在植物地上与地下部分的含量均在p H 4.0时最大。T2处理时东南景天在p H 4.0时体内重金属含量最高,但由于植物生长受到Al和Mn等元素的毒害,此时生物量最小。东南景天对土壤重金属去除率均在p H 5.5时最高,其中T1处理时Cd、Zn去除率分别为16%和1.33%,T2处理时分别为27%和1.09%;2种污染水平土壤重金属的去除率均在p H 8.5时最小。因此,适当降低土壤p H,可有效提高植物积累和去除土壤Zn、Cd的效率。本研究为进一步利用东南景天修复重金属污染土壤、提高植物修复效率提供了科学依据。 相似文献
9.
宁夏引黄灌区猪粪还田对麦田土壤硝态氮淋失的影响 总被引:4,自引:0,他引:4
以宁夏引黄灌区为例,探索猪粪还田条件下冬小麦田土壤硝态氮淋失规律.试验设置3个处理:常规施化肥225 kg N·hm-2(CK)、常规施肥基础上施用4500 kg·hm-2(T1)和9000 kg·hm-2(T2)猪粪.利用树脂芯法吸附30、60和90 cm土层的硝态氮淋失量.结果表明:在常规施肥基础上增施猪粪,小麦生育期土壤硝态氮(纯N)淋失量为9.33~14.04kg·hm-2,占施N量的4.2%~6.2%.与CK相比,30 cm土层T1、T2的硝态氮淋失量增加2.6%和2.1%;60 cm土层增加1.5%和减少1.3%;90 cm土层减少8.7%和增加4.0%.增施猪粪与对照在30、60和90 cm土层处的硝态氮淋失量均无显著差异,而在深层土壤表现出减少趋势.硝态氮淋失主要发生在返青至灌浆期间,日均淋失量高于全生育期平均水平,该阶段的硝态氮淋失量占生育期内总淋失量的58.7%~75.3%.T1、T2春小麦产量比对照分别增加9.3%和12.5%. 相似文献
10.
湖南省4种森林群落土壤氮的矿化作用 总被引:9,自引:0,他引:9
2007年7月,用树脂芯原位测定土壤无机氮含量的方法,对湖南杉木、马尾松、樟树和枫香4种森林群落的土壤氮矿化进行了研究.研究结果表明,经过28d培养,4种森林群落土壤中NH+4-N含量分别下降了31.4%~50.5%,NO-3-N含量增加了8.2~17.3倍,氮矿化主要表现为硝化作用;氮矿化速率由大到小依次为樟树(0.05mg·kg-1·d-1)>马尾松(0.04 mg·kg-1·d-1)>枫香(-0.12 mg·kg-1·d-1)>杉木(-0.15 mg·kg-1·d-1).在4个森林群落的土壤中,NH+4-N是无机氮的主要存在形式,表现为在杉木群落中占78.42%、在马尾松中占79.17%、在樟树中占71.14%和枫香中占79.22%,而且NH+4-N的变化可以解释氮矿化量变化的96.1%~98.8%.土壤氮矿化速率与0~15 cm土壤的C/N、pH值呈显著性正相关,但与凋落物量和0~30 cm 土壤中细根生物量相关性不显著. 相似文献
11.
亚热带不同林分土壤矿质氮库及氮矿化速率的季节动态 总被引:4,自引:0,他引:4
以亚热带地区天然林、格氏栲人工林和杉木人工林为对象,采取PVC管原位培养连续取样法,对不同林分土壤净氨化速率、净硝化速率及净氮矿化速率进行为期一年(2014年9月—2015年8月)的研究,分析林分类型和季节动态对土壤矿质氮库和净氮矿化速率的影响.结果表明: 硝态氮是该地区土壤矿质氮库的主要存在形式,天然林和杉木人工林土壤硝态氮含量分别占总土壤矿质氮库的55.1%~87.5%和56.1%~79.1%,林分间土壤铵态氮含量差异不显著,硝态氮含量差异显著,其中格氏栲人工林土壤硝态氮含量显著低于天然林和杉木人工林.土壤硝态氮库和矿质氮库在不同月份间差异显著,在植物非生长季节(10月至次年2月)较大,在植物生长季节(3—9月)较小.各林分全年土壤净硝化速率均较低,净氨化速率是净氮矿化速率的主要存在形式,林分类型对土壤净氨化速率有显著影响,其中杉木人工林显著低于天然林和格氏栲人工林.月份对土壤净氨化速率有显著影响,各林分土壤净氨化速率变化规律不一致,但均在11月和2月达到一年中的最低值.重复测量方差分析显示,林分类型和季节动态对土壤矿质氮库及氮矿化速率均有显著影响.温度和水分是影响土壤矿质库及氮矿化速率的重要因素,凋落物对土壤氮矿化速率的影响主要是通过质量控制而非数量控制. 相似文献
12.
Elevated temperature increases the accumulation of microbial necromass nitrogen in soil via increasing microbial turnover 总被引:1,自引:0,他引:1
Xu Wang Chao Wang M. Francesca Cotrufo Lifei Sun Ping Jiang Ziping Liu Edith Bai 《Global Change Biology》2020,26(9):5277-5289
Microbial‐derived nitrogen (N) is now recognized as an important source of soil organic N. However, the mechanisms that govern the production of microbial necromass N, its turnover, and stabilization in soil remain poorly understood. To assess the effects of elevated temperature on bacterial and fungal necromass N production, turnover, and stabilization, we incubated 15N‐labeled bacterial and fungal necromass under optimum moisture conditions at 10°C, 15°C, and 25°C. We developed a new 15N tracing model to calculate the production and mineralization rates of necromass N. Our results showed that bacterial and fungal necromass N had similar mineralization rates, despite their contrasting chemistry. Most bacterial and fungal necromass 15N was recovered in the mineral‐associated organic matter fraction through microbial anabolism, suggesting that mineral association plays an important role in stabilizing necromass N in soil, independently of necromass chemistry. Elevated temperature significantly increased the accumulation of necromass N in soil, due to the relatively higher microbial turnover and production of necromass N with increasing temperature than the increases in microbial necromass N mineralization. In conclusion, we found elevated temperature may increase the contribution of microbial necromass N to mineral‐stabilized soil organic N. 相似文献
13.
Nitrogen transformation rates are affected by cover soil type but not coarse woody debris application in reclaimed oil sands soils
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Forest floor mineral soil mix (FMM) and peat mineral soil mix (PMM) are cover soils commonly used for reclamation of open‐pit oil sands mining disturbed land in northern Alberta, Canada; coarse woody debris (CWD) is another source of organic matter for land reclamation. We investigated net nitrogen (N) transformation rates in FMM and PMM cover soils near and away from CWD 4–6 years after oil sands reclamation. Monthly net nitrification and N mineralization rates varied over time; however, mean rates across the incubation periods and microbial biomass were greater (p < 0.05) in FMM than in PMM. Net N mineralization rates were positively related to soil temperature (p < 0.001) and microbial biomass carbon (p = 0.045). Net N transformation rates and inorganic N concentrations were not affected by CWD; however, the greater 15N isotope ratio of ammonium near CWD than away from CWD indicates that CWD application increased both gross N mineralization/nitrification (causing N isotope fractionation) and gross N immobilization (no isotopic fractionation). Microbial biomass was greater near CWD than away from CWD, indicating the greater potential for N immobilization near CWD. We conclude that (1) CWD application affected soil microbial properties and would create spatial variability and diverse microsites and (2) cover soil type and CWD application had differential effects on net N transformation rates. Applying FMM with CWD for oil sands reclamation is recommended to increase N availability and microsites. 相似文献
14.
以长白山阔叶红松混交林为研究对象,于2006—2008年原位模拟不同形态氮((NH4)2SO4、NH4Cl和KNO3)沉降水平(22.5和45kgN·hm-2·a-1),利用树脂芯法技术(resin-core incubation technique)测定了表层(有机层0~7cm)和土层(0~15cm)土壤氮素净矿化、净氨化和净硝化通量的季节和年际变化规律。同时,结合前人报道的有关林地碳、氮过程及其环境变化影响的结果,力求有效预估森林生态系统中氮素年矿化通量对大气氮沉降量和水热条件等因子变化的响应。结果表明,长白山阔叶红松林地土壤氮素年净矿化通量为1.2~19.8kgN·hm-2·a-1,2008年不同深度的土壤氮素年净矿化通量均显著高于2006和2007年(P<0.05)。随着模拟氮沉降量增加,土壤氮素净矿化通量也随之增加,尤其外源NH4+-N输入对净矿化通量的促进作用更为明显(P<0.05),但随着施肥年限的延长,这种促进作用逐渐减弱。与林地0~15cm土壤相比,氮沉降增加对0~7cm有机层氮素净氨化和净矿化通量的促进作用更为明显,尤其NH4Cl处理的促进作用更大。结合前人报道的野外原位观测结果,土壤氮素年净矿化通量随氮素沉降量的增加而增大,氮沉降量对不同区域森林土壤氮素净矿化通量的贡献率约为52%;氮沉降量(x1)和pH值(x2)可以解释区域森林土壤氮素年净矿化通量(y)变化的70%(y=0.54x1-18.38x2-109.55,R2=0.70,P<0.0001)。前人研究结果仅提供区域年均温度,未考虑积温的影响,这可能是造成年净矿化通量与温度无关的原因。今后的研究工作应该加强区域森林土壤积温观测,进而更加准确地预估森林土壤氮素的年净矿化通量。 相似文献
15.
16.
Effects of precipitation intensity and temporal pattern on soil nitrogen mineralization in a typical steppe of Nei Mongol grassland
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《植物生态学报》2017,41(9):938
Aims Our objective is to: 1) explore the dynamics of soil nitrogen (N) mineralization in a grassland ecosystem in response to the changes in precipitation intensity and temporal distribution, and 2) identify the controlling factors.Methods The two study sites located in a typical steppe of the Nei Mongol grassland were fenced in 2013 and 1999, respectively. Our field experiment includes manipulations of three levels of precipitation intensity (increased 50%, decreased 50%, control) in three temporal patterns (increased or decreased precipitation for three years; increased or decreased precipitation for two years and no manipulation for one year; increased or decreased precipitation for one year and no manipulation for one year).Important findings 1) The soil net N mineralization and net nitrification rates decreased with changes in the temporal distributions of precipitation from one year to three years, with the maximum values of soil net N mineralization and nitrification rates observed in the treatments of increased or decreased precipitation for one year and no manipulation for one year (+PY1 or -PY1). This indicates that the high precipitation intensity and longer precipitation may have negative effects on soil net N mineralization and nitrification rates, while the moderate soilmoisture and temperature may stimulate soil mineralization. 2) The soil net N mineralization and nitrification rates, soil cumulative N mineralization, and nitrification in the fenced site in 1999 were higher than those in the site fenced in 2013, implying that a long-term enclosure may have promoted nutrient storage and soil quality restoration. 3) The long-term treatments of increased or decreased precipitation had significant effects on soil water content and temperature, whereas the short-term, discontinuous precipitation produced minor effects on soil moisture and temperature. Moreover, the controlling factors for soil N mineralization were different between the two fields. Soil moisture had a major effect on soil inorganic N content and net N mineralization rate in the site fenced in 2013, while soil temperature played a dominant role in the site fenced in 1999, with the net N mineralization rate depressed by higher soil moisture. Our findings suggest that the precipitation intensity and temporal distribution had important impacts on soil N mineralization in the Inner Mongolia grassland; these effects was site-dependent and particularly related to soil texture, community composition, and disturbance, and other factors. 相似文献
17.
Seasonal patterns of ammonium and nitrate uptake in nine temperate forest ecosystems 总被引:11,自引:2,他引:9
Summary Seasonal patterns of net N mineralization and nitrification in the 0–10 cm mineral soil of 9 temperate forest sites were analyzed using approximately monthlyin situ soil incubations. Measured nitrification rates in incubated soils were found to be good estimates of nitrification in surrounding forest soils. Monthly net N mineralization rates and pools of ammonium-N in soil fluctuated during the growing season at all sites. Nitrate-N pools in soil were generally smaller than ammonium-N pools and monthly nitrification rates were less variable than net N mineralization rates. Nitrate supplied most of the N taken up annually by vegetation at 8 of the 9 sites. Furthermore, despite the large fluctuations in ammonium-N pools and monthly net N mineralization, nitrate was taken up at relatively uniform rates during the growing season at most sites. 相似文献
18.
In an effort to elucidate the factors affecting soil N dynamics in the Dry Chaco ecosystem, soil respiration and microbial biomass N were measured for one year underneath 5 vegetation types: a leguminous tree (Prosopis flexuosa DC), a non-leguminous tree (Aspidosperma quebracho-blanco Schlecht.), a non leguminous shrub (Larrea spp.), the open interspaces, and a pure grassland. Ammonifier and nitrifier densities and N content in litter were also measured in some cases. Results were compared with previously reported N mineralization rates and soil fertility.During the dry season microbial biomass N and net N mineralization were low, while accretion of easily mineralizable C occurred (estimated through soil respiration rates in lab under controlled temperature and moisture). With the onset of rain, microbial biomass N and N mineralization increased markedly, resulting in a decrease in easily mineralizable C. Throughout the wet season N mineralization varied with soil moisture while microbial biomass N remained consistently high. Mean values of immobilized N in this ecosystem were high (20–140 mg kg–1), of about the same order of magnitude as accumulated net N mineralization (50–150 mg kg–1 yr–1). Microbial decay in the dry season, considered as a source of easily mineralizable N, accounted for only 40% of gross N mineralization increase at the beginning of the wet season. Ammonifier densities correlated significantly with soil moisture and N mineralization, but nitrifiers did not.The highest values of total N, N mineralization, inorganic N, microbial biomass N, nitrifier densities, N content in litter, total organic C and easily mineralizable C were found under Prosopis and the lowest values under shrubs and the interspaces. The main differences between tree species were in N mineralization at the beginning of the wet season, in total and inorganic N pools, and in nitrifier densities; all of which were significantly lower under Aspidosperma than under Prosopis.N mineralization in the pure grassland was very low despite high values of total N and C sources. Although N immobilized in microbial biomass was similarly high under Aspidosperma, Prosopis and the pure grassland, net N mineralization rates were quite different. 相似文献
19.
Effect of simulated forest fire on the availability of N and P in mediterranean soils 总被引:4,自引:0,他引:4
The effect of soil burning on N and P availability and on mineralization and nitrification rates of N in the burned mineral
soil was studied by combustion of soils in the laboratory.
At a fire temperature of 600°C, there was a complete volatilization of NH4 and a significant increase of pH, from 7.6 in the unburned soil to 11.7 in the burned soil. Under such conditions ammonification
and nitrification reactions were inhibited. Less available P was produced immediately after the fire at 600°C, as compared
to P amount produced at 250°C. Burning the soils with plants caused a decrease in NH4-N and (NO2+NO3)-N concentrations in the soil as well as a reduction in ammonification and nitrification rates. Combustion of soil with plants
contributed additional available P to the burned soil.
The existence of a non-burned soil under the burned one played an important role in triggering ammonification and nitrification
reactions. 相似文献
20.
En-Rong Yan Ya-Lin Hu Francis Salifu Xiao Tan Z. Chi Chen Scott X. Chang 《Plant and Soil》2012,359(1-2):215-231