Carbon and nitrogen dynamics in early stages of forest litter decomposition as affected by nitrogen addition

The effects of nitrogen （N） availability and tree species on the dynamics of carbon and nitrogen at early stage of decomposition of forest litter were studied in a 13-week laboratory incubation experiment. Fresh litter samples including needle litter （Pinus koraiensis） and two types of broadleaf litters （Quercus mongolica and Tilia amurensis） were collected from a broadleaf-korean pine mixed forest in the northern slope of Changbai Mountain （China）. Different doses of N （equal to 0, 30 and 50 kg.ha^-1yr^-1, respectively, as NH4NO3） were added to litter during the experiment period. The litter decomposition rate expressed as mass loss and respiration rate increased significantly with increasing N availability. The mass loss and cumulative CO2-C emission were higher in leaf litter compared to that in needle litter. The dis- solved organic Carbon （DOC） concentrations in litter leachate varied widely between the species, but were not greatly affected by N treatments. Regardless of the N addition rate, both N treatments and species had no significant effect on dissolved organic N （DON） concentrations in litter leachate. About 52-78% of added N was retained in the litter. The percentage of N retention was positively correlated （R^2=0.9 1, p〈0.05） with the litter mass loss. This suggested that a forest floor with easily decomposed litter might have higher potential N sink strength than that with more slowly decomposed litter.

Integration of nitrogen dynamics into the land surface model AVIM.Part 2:baseline data and variation of carbon and nitrogen fluxes in China

The spatiotemporal features of carbon and nitrogen fluxes over China between 1979 and 2015were simulated by the Atmosphere–Vegetation Interaction Model(AVIM).The carbon fluxes of gross primary production and net primary production captured the distribution pattern in China better than MODIS and TRENDY data.The results for nitrogen deposition and biological nitrogen fixation show the good performance of the AVIM simulation compared with the CMIP6 and CABLE data,with a deposition rate>4 g N m-2yr-1in south China.The variation in the gross primary production and net primary production can be up to 300 and 200 g C m-2yr-1in south and southeast China,respectively,and there is a discrepancy between the AVIM and the data from MODIS and TRENDY.This shows the difficulty in simulating the carbon flux in a monsoon climate region and the importance of coupling the nitrogen–carbon fluxes.The standard deviation of nitrogen deposition and biological nitrogen fixation is simulated well by the AVIM and there is a large range in nitrogen deposition of 0.8–1.2 g N m-2yr-1in south China.The climatological mean of the fluxes performs better than the variation in the standard deviation and anomaly and this variation in the carbon–nitrogen flux is the key to decreasing bias in future modeling studies.

Carbon and nitrogen dynamics in early stages of forest litter decomposition as affected by nitrogen addition

The effects of nitrogen(N) availability and tree species on the dynamics of carbon and nitrogen at early stage of decomposition of forest litter were studied in a 13-week laboratory incubation experiment.Fresh litter samples including needle litter(Pinus koraiensis) and two types of broadleaf litters(Quercus mongolica and Tilia amurensis) were collected from a broadleaf-korean pine mixed forest in the northern slope of Changbai Mountain(China).Different doses of N(equal to 0, 30 and 50 kg·ha-1yr-1, respectively, as NH4NO3) were added to litter during the experiment period.The litter decomposition rate expressed as mass loss and respiration rate increased significantly with increasing N availability.The mass loss and cumulative CO2-C emission were higher in leaf litter compared to that in needle litter.The dissolved organic Carbon(DOC) concentrations in litter leachate varied widely between the species, but were not greatly affected by N treatments.Regardless of the N addition rate, both N treatments and species had no significant effect on dissolved organic N(DON) concentrations in litter leachate.About 52?78% of added N was retained in the litter.The percentage of N retention was positively correlated(R2=0.91, p<0.05) with the litter mass loss.This suggested that a forest floor with easily decomposed litter might have higher potential N sink strength than that with more slowly decomposed litter.

Effects of nitrogen deposition on the carbon budget and water stress in Central Asia under climate change

Atmospheric deposition of nitrogen(N)plays a significant role in shaping the structure and functioning of various terrestrial ecosystems worldwide.However,the magnitude of N deposition on grassland ecosystems in Central Asia still remains highly uncertain.In this study,a multi-data approach was adopted to analyze the distribution and amplitude of N deposition effects in Central Asia from 1979 to 2014 using a process-based denitrification decomposition(DNDC)model.Results showed that total vegetation carbon(C)in Central Asia was 0.35(±0.09)Pg C/a and the averaged water stress index(WSI)was 0.20(±0.02)for the whole area.Increasing N deposition led to an increase in the vegetation C of 65.56(±83.03)Tg C and slightly decreased water stress in Central Asia.Findings of this study will expand both our understanding and predictive capacity of C characteristics under future increases in N deposition,and also serve as a valuable reference for decision-making regarding water resources management and climate change mitigation in arid and semi-arid areas globally.

The integration of nitrogen dynamics into a land surface model. Part 1: model description and site-scale validation

Nitrogen cycling has profound effects on carbon uptake in the terrestrial ecosystem and the response of the biosphere to climate changes.However,nutrient cycling is not taken into account in most land surface models for climate change.In this study,a nitrogen model,based on nitrogen transformation processes and nitrogen fluxes exchange between the atmosphere and terrestrial ecosystem,was incorporated into the Atmosphere–Vegetation Interaction Model(AVIM)to simulate the carbon cycle under nitrogen limitation.This new model,AVIM-CN,was evaluated against site-scale eddy covariance–based measurements of an alpine meadow located at Damxung station from the FLUXNET 2015 dataset.Results showed that the annual mean gross primary production simulated by AVIM-CN(0.7073 gC m^-2 d^-1)was in better agreement with the corresponding flux data(0.5407 gC m^-2 d^-1)than the original AVIM(1.1403 gC m^-2 d^-1)at Damxung station.Similarly,ecosystem respiration was also down-regulated,from 1.7695 gC m^-2 d^-1 to 1.0572 gC m^-2 d^-1,after the nitrogen processes were introduced,and the latter was closer to the observed vales(0.8034 gC m^-2 d^-1).Overall,the new results were more consistent with the daily time series of carbon and energy fluxes of observations compared to the former version without nitrogen dynamics.A model that does not incorporate the limitation effects of nitrogen nutrient availability will probably overestimate carbon fluxes by about 40%.

STUDIES ON THE DYNAMIC COMPETITIVE ADSORPTION OF ORGANIC VAPORS ON THE ACTIVATED CARBON FIBERS ACTIVATED WITH PHOSPHORIC ACID

The dynamic competitive adsorption behaviors of different binary organic vapor mixtures on ACF-Ps under different operation conditions were investigated by gas chromatography in this paper. The studied mixtures included benzene/toluene, toluene/xylene, benzene/isopropylbenzene, ethyl acetate/toluene and benzene/ethyl acetate. Experimental results show that various ACF-Ps, as with ACF-W, can remove both vapors in binary vapor mixtures with over 99% of removal efficiency before the breakthrough point of the more weakly adsorbed vapor. In dynamic competitive adsorption, the more weakly adsorbed vapor not only penetrates early, but also will be displaced and desorbed consequently by stronger adsorbate and therefore produces a rolling up in the breakthrough curve. The ACF-Ps prepared at different temperatures have somewhat different adsorption selectivity. The feed concentration ratio of vapors, the length/diameter ratio and the thick of bed have effect on competitive adsorption. The competitive adsorption ability of a vapor is mainly related to its boiling point. Usually, the higher the boiling point, the stronger the vapor adsorbed on ACF-P.

Changes of soil organic carbon and nitrogen in forage grass fields,citrus orchard and coniferous forests

Dynamic quantitative assessment of soil organic C and N is an available approach to understand the exact impact of land management on soils fertility. In this study the biomass of plants and content of soil organic C and N were compared in four typical land use systems which were planted with Ryegrass (Lolium multiflorum Lam.), Bahiagrass (Paspalum notatum Flugge.), Citrus (Citrus reticulata Blanco.), and Masson pine (Pinus Massoniana Lamb.) during 10 years in south China. Although biomass of plants in these four land use systems was nearly at the same level in the former investigation, total biomass for Ryegrass (RG), Bahiagrass (BG) was 3.68 and 3.75 times higher than that for Citrus (CT), and 2.06 and 2.14 times higher than that for Masson pine (MP) over 10 years of cultivation, respectively. Especially, underground total biomass for both RG and BG was over 10 times larger than that for CT and MP, indicating that forage grasses was much more beneficial to increase organic C and N storage in soils than CT and MP. The change content of soil organic C and N mainly occurred within soil depth of the 0–40 cm. The increased content of soil organic carbon and nitrogen was for 1.5 t·hm?2 and 0.2 t·hm?2 in the soil with planting RG and BG, and was for 1.2 t·hm?2 and 0.02 t·hm?2 in the soil with planting CT. An average loss was for 0.4 t·hm?2 and 0.04 t·hm?2 in the soil with planting MP during 10-year period. Keywords Soil organic carbon - Soil organic nitrogen - Dynamic change - Land use - Quantitative assessment CLC number S153.61 Document code A Foundation item: This research was partly supported by National Natural Science Foundation of China (30100144), and by Scientific Committee of Shenyang City (1011501900).Biography: WANG Xiao-ju (1967-), mail, Ph.D. Researcher in Center for Environmental Science in Saitama. Saitama Prefecture 347 0115, Japan.Responsible editor: Zhu Hong

Construction of Hierarchical Nanostructured N-doped TiO2 Immobilized Activated Carbon Fiber Porous Composites for Toluene Removal

The hierarchical nanostructured N-doped TiO2 immobilized activated carbon fiber(N-TiO2/ACF)porous composites are fabricated to removal dynamic toluene gas.The results show that nitrogen ions doping and ACF modification can decrease the band gap of TiO2,leading to red shift toward visible light region.Interestingly,N-TiO2/ACF exhibits strongly synergistic effect owing to high surface area,good crystallinity,enhanced bandgap structure and light harvesting.The toluene removal rate of N-TiO2/ACF composites is 2.29 times higher than that of TiO2.The N-TiO2/ACF for toluene degradation followed the Langmuir-Hinshelwood kinetic model,and the rate constant is enhanced 8 times compared with TiO2.The possible photodegradation pathway and mechanisms are proposed.

南亚热带常绿阔叶林土壤微生物生物量碳氮年际动态特征及其影响因子

土壤微生物是土壤有机质和养分循环的主要驱动者,研究土壤微生物生物量碳氮变化、稳态特征及其对环境因子内在的长期响应机理具有重要意义。以南亚热带常绿阔叶林土壤为对象,对土壤微生物生物量碳和氮(MBC和MBN)、土壤有机碳(SOC)、总氮(TN)、总磷(TP)、可溶性碳(ROC)、速效氮(AN)、pH、土壤温度(ST)和土壤含水量(SWC)进行连续10年监测;应用方差分析、相关性和回归分析及稳态分析等探究MBC和MBN的年际变化和稳态特征及主要影响因素。研究结果表明:(1)旱季MBC和MBN含量分别在171.32—358.45和25.90—54.08 mg/kg区间波动,雨季分别在394.01—507.97和68.40—88.05 mg/kg区间波动;旱、雨季的MBC含量年际间变化显著(P<0.05),但MBN含量仅在旱季变化显著(P<0.05)。雨季MBC和MBN含量均显著高于旱季(P<0.01),且雨季的MBC和MBN含量是旱季的2倍以上。(2)旱、雨季的MBC与MBN之间均呈显著正相关(P<0.05)。在旱季,MBC和MBN均与ROC和AN含量显著正相关(P<0.05),此外,MBN含量也与TP(P<0.05)和SOC(P<0.01)显著正相关。在雨季,仅SOC与MBN呈显著正相关(P<0.05)。(3)在旱季,MBC含量变化主要受ROC(P<0.05)和AN(P<0.001)影响,MBN则受AN控制(P<0.05)。在雨季,AN(P<0.05)主导了MBC的变化,TP(P<0.05)和SOC(P<0.05)是MBN变异的主导因子。AN(P<0.001)和SOC(P<0.001)是旱、雨季土壤MBC和MBN变化的主导因子。(4)土壤MBC和MBC/MBN稳态指数在年际间均为绝对稳态型(P>0.05);雨季的MBN(P=0.685)为绝对稳态型,但旱季为非稳态(P<0.01,H>1)。雨季微生物熵显著高于旱季(P<0.01),表明土壤有机质质量及养分利用效率更高。综上,MBC和MBN含量受季节更替显著影响,且主要受土壤SOC和AN的影响;受旱季水分限制,MBN的稳态更差。

基于DNDC模型分析氮添加对内蒙古草甸和荒漠草地碳动态的影响

[目的]确定内蒙古不同草地类型在氮沉降背景下植物生物量碳和土壤有机碳的变化,探究DNDC模型对该区域草地碳动态模拟的适用度,对减缓气候变化和实现“双碳”目标具有重要意义。[方法]通过调查内蒙古草甸和荒漠草地对氮沉降的响应,并利用DNDC模型进行模拟验证。设置不同氮添加梯度[0,5,10,15,20,25,30 gN/(m^(2)·a)],分析了氮添加对不同草地碳库的影响,评估了DNDC模型对其模拟的差异。[结果](1)与空白对照相比,氮添加对草甸草地和荒漠草地地上生物量碳具有促进作用,平均分别增加了72.68%和66.52%,草甸草地在N_(5)处理下地下生物量碳达到最大值(240.93 gC/kg),荒漠草地则在N_(4)处理下增幅最大(129.67 gC/kg);(2)相对于对照组,氮添加对两种草地地下生物量碳没有显著影响,与地上生物量碳的响应不同,但整体而言,地下碳量表现为草甸草原>荒漠草原;(3)氮添加对两种草地土壤有机碳含量的影响均不显著,且不同氮添加处理间也没有显著性差异,总体而言,草甸草地土壤有机碳含量高于荒漠草地;(4) DNDC模型能够较好地模拟研究区草甸草地和荒漠草地的地上、地下生物量碳和土壤有机碳,模型的模拟值与实测值基本一致,决定系数R^(2)分别为0.9426,0.756 8,0.825 7,0.523 8,0.909 9,0.955 2,0.861 0,0.732 4,模型效率系数E分别为0.834 5,0.674 8,0.799 4,0.428 8,0.873 1,0.926 5,0.716 8,0.538 1,点位模拟效果整体良好,但对于生物量碳的模拟吻合程度更好,且对荒漠草原的模拟优于草甸草地。[结论]氮添加促进了不同干旱类型草地的固碳能力,DNDC模型能较好反映氮沉降对内蒙古两种类型草地的影响,因此模型可用于模拟内蒙古草地生态系统的生物量碳和土壤有机碳。

贵州喀斯特生态系统不同恢复阶段植物群落凋落物及碳氮归还动态

凋落物是森林生态系统碳库的重要组成部分,本研究对贵州普定喀斯特生态系统5种不同恢复阶段(稀灌草丛、藤刺灌丛、灌木林、乔灌过渡林、次生乔木林)植物群落的凋落物总量、凋落物组成(叶、枝、花果等)特征、凋落物量月动态及碳氮归还量进行了一年的定位观测。结果表明:稀灌草丛、藤刺灌丛、灌木林、乔灌过渡林、次生乔木林的年总凋落物量分别为726.0、3811.6、5161.0、4378.8、4604.8 kg/hm^(2),随着群落的恢复发展,凋落物总量呈现出先升高后缓降的变化趋势;各恢复阶段植物群落叶凋落物量占总凋落物量的64.2%~74.9%,枝凋落物量占总凋落物量的11.4%~18.1%,花果等凋落物量占总凋落物量的9.8%~19.5%;群落恢复初期(稀灌草丛、藤刺灌丛、灌木林)凋落物量月动态呈单峰型,而群落恢复中后期(乔灌过渡林、次生乔木林)凋落物量月动态呈双峰型,各恢复阶段植物群落的叶凋落物量与总凋落物量的月动态基本一致;C、N含量总体上表现为花果等凋落物>叶凋落物>枝凋落物,5种不同恢复阶段植物群落凋落物中C、N的年归还总量与其年总凋落物量显著正相关。

我国农田土壤碳氮耦合特征的区域差异

利用中国第2次土壤普查数据,分析了稻作和旱作方式下农田耕层土壤有机碳和全氮特征及其区域差异。结果表明,水田土壤有机碳和全氮含量分别为旱地的147.8%和145.5%,但水田碳氮含量的区域变异低于旱地。全国水田和旱地土壤有机碳氮比值分别为10.8和9.9,各区域水田土壤碳氮比值普遍高于旱地,其中东北水田最高,而华东旱地和西北旱地最低。旱地碳氮比值的区域变异显著,水田则不显著。农田耕层土壤有机碳和全氮含量呈显著正相关,除华北地区外,各区域无论水田还是旱地其碳氮含量之间相关系数都超过0.8,达极显著水平。由此可见,我国农田耕层土壤有机碳和全氮含量之间存在显著耦合关系,而且不同利用方式和区域之间差异显著;相同氮水平下,水田土壤可能储存更多的有机碳。

苏北潮滩湿地不同生态带碳、氮、磷分布特征

通过对比苏北潮滩湿地不同生态带的表层以及柱状沉积物中总有机碳、总氮、总磷和有机磷含量,并结合不同植被不同植株部位中碳、氮、磷的含量变化,分析了潮滩沉积物中碳、氮、磷的垂向和水平分布特征与规律,探讨了不同生态带以及潮滩植被对碳、氮、磷等生源要素的富集作用。对比分析结果表明:苏北潮滩湿地各生态带对不同的测量指标有着不同的富集作用,互花米草滩的总有机碳、总氮和有机磷含量要远大于其他几个生态带,光滩沉积物中总磷的含量最高;粒度效应是控制互花米草前缘地带以及互花米草滩沉积物中有机碳和氮分布的一个重要因素,盐蒿和芦苇滩中有机碳和氮的分布更多的是受粒度之外的其他因素影响;不同生态带表层沉积物中的C/N比值分布,大致可反映其有机物来源的差异,而不同生态带中柱状沉积物中的C/N比值相对接近,很难根据C/N比值大小来对不同生态带中的有机物来源进行判断,这可能是埋藏在柱状沉积物中的有机物更多的受到了早期成岩作用造成的。植被对潮滩湿地中碳、氮、磷的分布有着重要影响,3种物质在互花米草、盐蒿和芦苇中的含量差别不是很大,因此潮滩植被对沉积物中上述3种物质的贡献差别主要是由不同植被的生物量和其所处环境的沉积动力差异造成的。

青藏高原东部不同草地类型土壤养分的分布规律

调查分析了青藏高原东部高寒草甸、高寒灌丛草甸、亚高寒草甸、沼泽化草甸、荒漠化草原、林间草地、盐渍化沼泽土壤碳氮磷含量垂直分布特征。结果表明,7种草地类型中,土壤有机碳含量大体随着土层的深入而降低,0～15cm土层土壤有机碳的累积量从高到低依次为林间草地>高寒灌丛草甸>高寒草甸>沼泽化草甸>盐渍化沼泽>亚高寒草甸>荒漠化草甸(P<0.05);随土层深度变化土壤全氮含量与有机碳相似,0～15cm全氮累积量从高到低依次为沼泽化草甸>林间草地>高寒灌丛草甸>高寒草甸>盐渍化沼泽>荒漠化草原>亚高寒草甸(P<0.05);荒漠化草原、林间草地和土壤全磷含量随土层深度无明显规律性,0～15cm土层全磷累积量由高到低依次为高寒灌丛草甸>沼泽化草甸>高寒草甸>盐渍化沼泽>亚高寒草甸>荒漠化草原>林间草地(P<0.05);随土层深度的增加不同草地类型养分含量顺序不同。除沼泽化草甸,不同草地类型下土壤有机碳与全氮呈显著正相关。

炭化小麦秸秆对水中氨氮吸附性能的研究

用直接炭化法制备了小麦秸秆吸附剂,并通过静态吸附试验研究了炭化小麦秸秆对氨氮的吸附性能和影响因素。结果表明:直接炭化法制备小麦秸秆吸附剂的最佳炭化温度为300℃;在试验的pH值范围内,pH=9时炭化小麦秸秆对氨氮的吸附去除最好;300℃时炭化小麦秸秆吸附不同质量浓度(ρ=30 mg/L、50 mg/L、100 mg/L)氨氮的动力学曲线符合准二级动力学模型,吸附常数k2分别为0.681 8g/(mg.min)、0.747 4 g/(mg.min)、1.025 0 g/(mg.min);直接炭化小麦秸秆吸附剂对氨氮吸附去除的最佳温度是30℃;不同温度下的吸附等温线可用Freundlich吸附等温方程进行拟合;由吸附热力学方程计算得到的等量吸附焓变ΔH>0,吸附自由能变ΔG<0,吸附熵变ΔS>0,表明炭化小麦秸秆对氨氮的吸附为吸热的和熵增加的自发过程,且属于物理吸附。

A-A^2/O工艺处理低碳源城市污水的除磷脱氮效果

文章以南方某污水处理厂的实际运行情况为例,介绍了A-A2/O工艺在处理低碳源城市污水的效果。运行结果表明,工艺对BOD5、COD、SS的去除效果良好,达到《城镇污水处理厂污染物排放标准》(GB18918-2002)一级A标准。对于氮磷去除,出水NH4-N<0.5mg/L,TN<15mg/L,TP<1.5mg/L,但TN平均去除率只有45%左右;TP大多数的去除率在30%～50%之间。造成这种结果的主要原因是碳源不足。为提高除磷脱氮效果,采取了投加PAC来辅助除磷,并提出了进一步的改进措施,供同行参考。

山东南部近海沉积物中碳、氮、磷的分布特征

对山东近海31个站位表层沉积物中的总氮、总磷和总有机碳的含量和分布特征进行了研究。结果表明,总氮、总磷和总有机碳含量均较低,高值区主要分布在胶州湾及湾口和北部海域,总氮浓度范围为0.31～0.75mg/g,平均值为0.52mg/g,总磷浓度范围为0.18～0.32mg/g,平均值为0.24mg/g,总有机碳浓度范围为0.17%～0.49%,平均值为0.33%。相关性分析表明,总氮和总有机碳的相关性较好,总有机碳和总氮比值(TOC/TN)略高于Redfield比值,表明这两种生源要素的来源可能是一致的。

森林土壤微生物生物量动态变化研究进展

土壤微生物生物量是土壤有机质中最为活跃的部分,它调节着陆地生态系统的生物地球化学过程。不少研究表明,森林土壤微生物生物量具有明显的季节动态变化特征。本文在综合前人研究的基础上,对森林土壤微生物生物量的季节动态变化规律及其影响因子进行了归纳和总结,发现森林土壤微生物生物量的季节波动主要有夏高冬低型、夏低冬高型和干-湿季节交替循环型3种模式,这些变化类型主要与土壤温度、土壤湿度、季节干-湿交替循环或与植物的生长节律等有关。在今后的相关研究中,要加强对森林土壤微生物生物量季节动态变化调控机理的研究,并注重对土壤微生物生物量C与土壤微生物生物量N、P动态变化的耦合关系的研究。

毛乌素沙地湖滨带沉积物碳氮磷生态化学计量学特征

为了阐明毛乌素沙地湖滨带沉积物生态化学计量学特征及其指示意义,对不同类型区湖滨带沉积物有机碳、全氮和全磷含量进行了测定与分析。结果表明:不同类型区湖滨带沉积物有机碳和全氮含量变化趋势一致,表现为距离湖泊中心位置愈远其含量愈低;湖滨带沉积物有机碳、全氮、全磷含量剖面分布具有一定层次性,表现为0—10cm>10—20cm>20—40cm,湖滨带沉积物全磷的变化相对滞后于有机碳和全氮,其水平分布特征与有机碳和全氮不同,剖面分布相似;土壤含水率和土壤容重是影响沉积物养分分布的关键因子,同时也是影响C/P和N/P变化的主要因素;生态化学计量学特征分析表明,除相对远离湖泊中心的类型区C/N和C/P与土壤碳储量的变化趋势一致外,靠近湖泊中心的类型区碳与养分比值未表现出对土壤碳储量良好的指示作用。

不同退化程度的草地植被和土壤特征

研究了克氏针茅(Stipa krylovii)草原未退化、中度退化和重度退化草地的植被和土壤微生物的季节动态。结果表明,随退化程度增加,克氏针茅的重要值降低,冷蒿(Artemisia frigida)的重要值增加,重度退化草地群落多样性最低。重度退化草地土壤全氮含量最高而有效磷含量最低。未退化草地土壤微生物碳、氮含量高于退化草地,草地退化对菌根真菌(AMF)孢子密度、细菌、真菌和放线菌数量的影响随季节变化而不同。5―8月未退化草地真菌数量大于重度退化草地,9月两者差异不显著。7―9月未退化草地细菌数量大于重度退化草地,6月两者差异不显著。各指标均在7月或8月达到最高值。土壤真菌、细菌、放线菌与土壤全氮、微生物氮均有显著相关性。土壤真菌、细菌与土壤微生物碳有显著相关性。