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1.
Philip模型参数推求湿润锋平均基质吸力Sf准确性   总被引:7,自引:1,他引:6  
修改的适用自然降水入渗的Green—Ampt模型是模拟坡面降水入渗、产汇流的常用手段,该模型中一个重要参数——湿润锋平均基质吸力Sf的准确取值对提高计算精度有重要作用。在分析Philip入渗模型和Green—Ampt入渗模型的基础上,建立了两模型参数间的转化关系,并尝试用Philip模型参数间接推求Green—Ampt模型中的参数Sf。通过对积水入渗资料的处理和用降水产流资料进行准确性检验,结果发现,对黄土高原黑垆土而言,用Philip模型参数间接推求Green—Ampt模型中的湿润锋平均基质吸力Sf是可行的,与直接用Green—Ampt模型获得的Sf值具有相同的精度。  相似文献   

2.
为进一步探究盐碱土的入渗机理,实现科学的盐碱土农业生产与灌溉,基于传统Green-Ampt模型,根据盐碱土的入渗特性引进扩散率D(θ),并结合对土壤剖面含水量分布的划分假定对模型进行修正。利用5种盐碱土进行一维积水入渗试验,采用入渗率、湿润锋数据验证该修正模型。结果显示:修正模型模拟值与实测值的一致性良好,进行相关分析得到5种盐碱土入渗率R2平均值为0.983,平均绝对误差均小于0.05;湿润锋R2平均值为0.868,平均绝对误差均小于3.50。将修正模型参数饱和导水率、湿润锋面基质吸力值与盐碱土盐分离子含量进行相关分析,结果显示基质吸力值随K++Na+含量的减少而减小,饱和导水率随K++Na+含量的减少而增大。该修正模型经验证可应用于不同盐渍化程度的盐碱土入渗过程模拟,从而为深入盐碱土水分入渗机制研究与加快盐碱土农业生产提供理论支持。  相似文献   

3.
羧甲基纤维素钠对壤砂土水分运动及水力参数的影响   总被引:1,自引:0,他引:1  
科学使用羧甲基纤维素钠(CMC)实现保水控盐对于滨海壤砂盐碱土改良具有重要意义,而明晰CMC对滨海壤砂土水分运动规律的影响是科学使用CMC的重要基础。为研究施加CMC滨海壤砂土水分运动规律,本文通过开展一维垂直土柱积水入渗试验,探索不同CMC施量(0、0.1、0.2、0.4、0.6 g?kg-1) 对壤砂土入渗特性、水分分布和土壤水力参数的影响。结果表明,施用CMC土壤的最终累积入渗量增加了4.90%~15.17%、达到预设湿润锋深度的入渗时间增加了61.90%~604.73%;Philip入渗模型参数吸渗率S和Green-Ampt模型参数KsSf均随CMC施量的增加而减少,吸渗率S和平均土壤水扩散率与CMC施量之间的数学关系分别可用二次多项式和指数函数来表示;CMC增强了土壤的持水能力,土壤剖面含水量提高了0.72%~3.74%;CMC通过改变土壤结构影响了土壤水力参数,滞留含水率θr、饱和含水率θs及进气吸力倒数α均与CMC施量呈正相关关系,而与饱和导水率Ks和形状系数n呈反比关系。通过对变异系数CV的分析发现,CMC对饱和导水率Ks和进气吸力倒数α影响表现为中等差异,对滞留含水率θr、饱和含水率θs和形状系数n表现为弱差异。研究结果揭示了CMC对滨海壤砂土减渗保水的内在机理,为滨海盐碱地的改良提供了理论参考。  相似文献   

4.
用土壤物理特性推求Green-Ampt入渗模型中吸力参数Sf   总被引:10,自引:1,他引:9  
张光辉  邵明安 《土壤学报》2000,37(4):553-557
Green-mpt模型是1911年由Green-Ampt基于毛管理论提出的入渗模型[1],国外在50年代就有广泛的应用,70年代以后又有了新的发展和完善。该模型形式简单,且具有一定的物理学基础。虽然 它是基于均质土壤推导而来,但70年代以后被普遍用于非均质土壤或初始含水量分布不均匀的情况,结果均较为满意[2]。土壤质地较为均一的假定对分布极广、水平层理发育较好的黄土是完全可以满足的。1973年Mein和Larson提出了将Green-Ampt模型应用于降雨入渗的研究领域,并推导出了相应的修正模型[3]。自此Green-Ampt模型被广泛应用于降雨入渗、坡面产流、土壤侵蚀预测预报模型等研究领域,在欧洲的LISEM模型[4]和美国的WEPP模型[5]中均有应用。实际应用Green朅mpt模型时,如何准确、迅速确定饱和导水率Ks和土壤吸力参数Sf具有一定的难度。一般Ks可用常水头法测定,而Sf则不易用实验直接测定,在国外一般先假定Sf值,利用土壤入渗试验结果进行反推,这种方法既费时费力,又精度不高,而在国内还没有现成的推求方法,从而限制了 Green-Ampt模型在我国的应用和发展。  相似文献   

5.
Green-Ampt模型参数简化及与土壤物理参数的关系   总被引:3,自引:3,他引:0  
简化模型表达形式从而减少参数个数,对于Green-Ampt入渗模型的实际应用具有重要的现实意义。该文通过推导湿润锋处平均基质吸力与Philip模型中土壤吸湿率关系基础上提出了简化的Green-Ampt入渗模型,基于新疆222兵团两块壤质土壤田块上土壤水分入渗试验资料,分析了Green-Ampt简化入渗模型参数与土壤物理参数之间的关系,建立了模型参数与土壤物理参数之间的定量经验转换函数。结果表明,入渗参数A(组合参数)与土壤初始含水率呈对数负相关,相关系数为0.77,A与土壤紧实度和黏粒含量均呈指数负相关,相关系数分别为0.70和0.74。饱和导水率Ks与土壤紧实度和黏粒呈指数负相关,相关系数分别为0.74和0.73。A和Ks与土壤初始含水率、土壤紧实度和黏粒含量呈高度和中度多元线性相关,相关系数分别为0.9和0.79。研究表明Green-Ampt简化入渗模型能够在一定精度下分析土壤入渗过程。  相似文献   

6.
间接地下滴灌土壤湿润体特征参数   总被引:4,自引:1,他引:3       下载免费PDF全文
该文将恒定水头钻孔积水入渗求解土壤饱和导水率的稳态原理用于定量化求解间接地下滴灌技术中与任意导水装置尺寸相匹配的滴头流量,并以计算的技术参数为基础,研究了间接地下滴灌水分运移过程中的土壤湿润体特征参数。研究结果表明,用于描述恒定水头钻孔积水入渗法求解土壤饱和导水率的稳态模型能够较好地设计与不同类型土壤和导水装置尺寸相匹配的适宜滴头流量。间接地下滴灌灌水过程中,从零开始逐渐增大并趋于稳定的积水深度加速了水分在垂直方向的运移,缩小了横向湿润距离和垂向湿润距离之间的差异,但变化的积水深度对湿润锋在垂直方向向上和向下的运移速率影响不大,使湿润体形状表现为扁率不断减小的椭球体,且椭球体对称轴分布在靠近导水装置底部的位置。湿润锋最大湿润距离和湿润体体积是灌水时间的函数,湿润体内平均体积含水率增量与灌水时间关系不大,保持为一定值。湿润体体积和湿润体内平均体积含水率增量不仅与土壤类型有关,还与导水装置参数和滴头流量的不同组合有关。  相似文献   

7.
基于Green-Ampt的膜孔灌三维入渗模型建立与验证   总被引:1,自引:0,他引:1  
在膜孔灌入渗方面研究中的入渗模型缺少明确的物理意义,针对这一问题,该文以一维Green-Ampt公式为基础进行探讨。对公式中概化湿润锋为平面的假设条件进行深化讨论,结合膜孔灌三维入渗特点,建立了包含膜孔直径、表征导水率和湿润锋面水吸力的膜孔灌入渗模型,利用室内入渗试验和以不同土壤质地(典型砂壤土、典型壤土和典型粉壤土)的Hydrus-2D软件数值模拟结果对其进行验证。结果表明:试验观测和数值模拟得到的单位面积累积入渗量随时间的变化规律与模型计算得出的结果一致,二者均方根误差和平均绝对误差接近于0,偏差百分比小于10%,数值相差不大;由模型计算得出的概化湿润锋由试验及模拟结果在入渗前期相差很小,在入渗后期差别逐渐变大;另外,相较于水平方向,垂直方向的概化湿润锋计算结果更加接近试验观测值和数值模拟值。建立的模型可为准确计算膜孔灌累积入渗量、预测湿润锋形状提供依据。  相似文献   

8.
为计算黄土高原3种土壤温度下的非饱和土壤导水率,采用土壤水分动力学方法和数值模拟,利用室内试验分别对3种土壤不同温度下的土壤水分特征曲线,湿润峰下渗速率以及湿润峰湿度与湿润剖面平均湿度的关系进行了定量研究,得到出了以下结果,(1)建立了黄土高原3种土壤非饱和土壤导水率温度效应的定量模型,K(θ)=△aθ^b+KTte,栖模型为了解田间土壤水分的动态变化及评价土壤水分有效性提供了理论依据,(2)在已有模型的基础上,计算了不同含水量,温度升高1℃所引起非饱和土壤导水率和土壤有效水的净增加量,并推导出更为直观的温度对土壤水分传导有效性影响的定量模型,可以直接计算不同温度下非饱和土壤导水率的温度效应。  相似文献   

9.
均质土微润灌湿润体模型构建及验证   总被引:2,自引:1,他引:1  
为探明微润灌土壤湿润体运移的影响因素和变化规律,设置了56种微润灌情景(8种土壤质地、3种土壤基质势和10种微润管比流量的不同组合),利用HYDRUS-2D软件,模拟研究土壤饱和导水率、土壤基质势和微润管比流量对微润灌土壤湿润体的影响。综合考虑单位长度总渗水量、土壤饱和导水率、土壤基质势和微润管比流量等影响因素,基于量纲分析方法,建立了一种均质土微润灌湿润体尺寸估算模型,并利用数值模拟结果,定量获取了所建模型的待定参数,最后,采用试验资料评价了估算模型的可靠性。结果表明,土壤饱和导水率、土壤基质势和微润管比流量对微润灌土壤湿润体形状影响较小,且在湿润锋未到达地表前,湿润体形状均为以线源为轴线的近似"椭圆柱体";相同土壤饱和导水率条件下,土壤湿润体水平、垂直向下和垂直向上方向上的湿润锋运移速率均随土壤基质势和微润管比流量增大而增大;当土壤基质势和微润管比流量恒定时,随土壤饱和导水率数值的增大,垂直向上和水平方向的湿润锋运移速率逐渐减小,而垂直向下的湿润锋运移速率存在先减小后增大的现象;所建模型的统计指标平均绝对误差、均方根误差均趋近于0,纳什效率接近1,说明模型估算效果良好,可为微润灌工程的运行及管理提供科学依据。  相似文献   

10.
添加γ-聚谷氨酸减少土壤水分深层渗漏提高持水能力   总被引:14,自引:3,他引:11  
γ-聚谷氨酸(Poly-γ-glutamic acid,γ-PGA)是一种高分子聚合物,具有超强的吸水能力和生物降解性。为探明γ-PGA在土壤改良方面的应用及对土壤水分运动的影响,该文基于室内垂直一维入渗土柱试验,研究了不同γ-PGA施量配比(0、0.5%、1%、2%、4%)对土壤水分入渗及持水特性的影响。结果表明:与对照组相比,添加4%的γ-PGA的累积入渗量、入渗率和湿润锋分别减少了57.95%、53.89%、59.58%;四种入渗模型参数的模拟结果显示,与对照组相比,随着γ-PGA施量的增加,Kostiakov公式中的经验系数从0.808减小到0.538,经验指数从0.530增大到0.623;Philip入渗公式中的吸渗率从0.704减小到0.292;Green-Ampt公式中,饱和导水率从0.0043减小到0.0011 cm/min,湿润区有效的土壤水扩散率从1.19减小到0.16 cm~2/min,湿润锋处的土壤水吸力无明显变化;垂直一维入渗代数模型中,饱和导水率从0.0044减小到0.001 cm/min,非饱和土壤吸力分配系数和土壤水分特征曲线和非饱和导水率综合形状系数均无明显变化趋势。土壤的持水特性结果表明:随着γ-PGA施量的增加,土壤饱和含水率增加,且与对照相比,表层土壤(0~10 cm土层)的含水率呈显著增加趋势,深层土壤(≥10~40 cm土层)的含水率则呈减小趋势。同时,湿润土层的厚度逐渐减小,说明γ-PGA不仅可增强土壤的持水能力,而且还可改变土壤剖面水分的分布形态,使更多水分蓄积在作物根区土层区域。该研究为γ-PGA的田间土壤改良及应用提供了理论支撑。  相似文献   

11.
The degradation rate of the pollutant is often an important parameter for designing and maintaining an active treatment system or for determining the rate of natural attenuation. A quasi‐steady‐state gas transport model based on Fick’s law with a correction term for advective flux, for estimating diesel degradation rates from N2, O2 and CO2 concentration versus depth data, was evaluated in a laboratory column study. A loamy sand was spiked with diesel fuel at 0, 1000, 5000 and 10 000 mg kg−1 soil (dry weight basis) and incubated for 15 weeks. Soil gas was sampled weekly at 6 selected depths in the columns and analysed for O2, CO2 and N2 concentrations. The agreement between the measured and the modelled concentrations was good for the untreated soil (R2= 0.60) and very good for the soil spiked with 1000 mg kg−1 (R2= 0.96) and 5000 mg kg−1 (R2= 0.97). Oxygen consumption ranged from −0.15 to −2.25 mol O2 m−3 soil day−1 and CO2 production ranged from 0.20 to 2.07 mol CO2 m−3 soil day−1. A significantly greater mean O2 consumption (P < 0.001) and CO2 production (P < 0.005) over time was observed for the soils spiked with diesel compared with the untreated soil, which suggests biodegradation of the diesel substrate. Diesel degradation rates calculated from respiration data were 1.5–2.1 times less than the change in total petroleum hydrocarbon content. The inability of this study to correlate respiration data to actual changes in diesel concentration could be explained by volatilization, long‐term sorption of diesel hydrocarbons to organic matter and incorporation of diesel hydrocarbons into microbial biomass, aspects of which require further investigation.  相似文献   

12.
Emissions of N2O and CH4 and CH4 oxidation rates were measured from Lolium perenne swards in a short-term study under ambient (36 Pa) and elevated (60 Pa) atmospheric CO2 at the Free Air Carbon dioxide Enrichment experiment, Eschikon, Switzerland. Elevated pCO2 increased (P<0.05) N2O emissions from high N fertilised (11.2 g N m−2) swards by 69%, but had no significant effect on net emissions of CH4. Application of 13C-CH4 (11 μl l−1; 11 at.% excess 13C) to closed chamber headspaces in microplots enabled determination of rates of 13C-CH4 oxidation even when net CH4 fluxes from main plots were positive. We found a significant interaction between fertiliser application rate and atmospheric pCO2 on 13C-CH4 oxidation rates that was attributed to differences in gross nitrification rates and C and N availability. CH4 oxidation was slower and thought to be temporarily inhibited in the high N ambient pCO2 sward. The most rapid CH4 oxidation of 14.6 μg 13C-CH4 m−2 h−1 was measured in the high fertilised elevated pCO2 sward, and we concluded that either elevated pCO2 had a stimulatory effect on CH4 oxidation or inhibition of oxidation following fertiliser application was lowered under elevated pCO2. Application of 14NH415NO3 and 15NH415NO3 (10 at.% excess 15N) to different replicates enabled determination of the respective contributions of nitrification and denitrification to N2O emissions. Inhibition of CH4 oxidation in the high fertilised ambient pCO2 sward, due to competition between NH3 and CH4 for methane monooxygenase enzymes or toxic effects of NH2OH or NO2 produced during nitrification, was hypothesised to increase gross nitrification (12.0 mg N kg dry soil−1) and N2O emissions during nitrification (327 mg 15N-N2O m−2 over 11 d). Our results indicate that increasing atmospheric concentrations of CO2 may increase emissions of N2O by denitrification, lower nitrification rates and either increase or decrease the ability of soil to act as a sink for atmospheric CH4 depending on fertiliser management.  相似文献   

13.
Relationship between soil CO2 concentrations and forest-floor CO2 effluxes   总被引:5,自引:2,他引:3  
To better understand the biotic and abiotic factors that control soil CO2 efflux, we compared seasonal and diurnal variations in simultaneously measured forest-floor CO2 effluxes and soil CO2 concentration profiles in a 54-year-old Douglas fir forest on the east coast of Vancouver Island. We used small solid-state infrared CO2 sensors for long-term continuous real-time measurement of CO2 concentrations at different depths, and measured half-hourly soil CO2 effluxes with an automated non-steady-state chamber. We describe a simple steady-state method to measure CO2 diffusivity in undisturbed soil cores. The method accounts for the CO2 production in the soil and uses an analytical solution to the diffusion equation. The diffusivity was related to air-filled porosity by a power law function, which was independent of soil depth. CO2 concentration at all depths increased with increase in soil temperature, likely due to a rise in CO2 production, and with increase in soil water content due to decreased diffusivity or increased CO2 production or both. It also increased with soil depth reaching almost 10 mmol mol−1 at the 50-cm depth. Annually, soil CO2 efflux was best described by an exponential function of soil temperature at the 5-cm depth, with the reference efflux at 10 °C (F10) of 2.6 μmol m−2 s−1 and the Q10 of 3.7. No evidence of displacement of CO2-rich soil air with rain was observed.Effluxes calculated from soil CO2 concentration gradients near the surface closely agreed with the measured effluxes. Calculations indicated that more than 75% of the soil CO2 efflux originated in the top 20 cm soil. Calculated CO2 production varied with soil temperature, soil water content and season, and when scaled to 10 °C also showed some diurnal variation. Soil CO2 efflux and concentrations as well as soil temperature at the 5-cm depth varied in phase. Changes in CO2 storage in the 0–50 cm soil layer were an order of magnitude smaller than measured effluxes. Soil CO2 efflux was proportional to CO2 concentration at the 50-cm depth with the slope determined by soil water content, which was consistent with a simple steady-state analytical model of diffusive transport of CO2 in the soil. The latter proved successful in calculating effluxes during 2004.  相似文献   

14.
[目的]研究陕西省延安地区重塑Q_3黄土高填方工程的后期沉降变形特性,为高填方工程的设计、施工提供一定的技术和理论支撑。[方法]通过改进K0三轴蠕变仪,对所取黄土进行了不同压实度、不同含水量、不同竖向应力下的室内土的静止侧压力系数K_0三轴固结排水蠕变试验。[结果]重塑Q_3黄土具有明显的蠕变特性,在低应力条件下,呈现出典型的衰减蠕变;在K_0条件下,随着含水量增大、竖向应力的增大,压实度的减小,蠕变呈增强趋势,蠕变变形量增大;在低水平应力的条件下,土体所受侧向应力与竖向应力成线性关系。[结论]建立了重塑Q_3黄土关于竖向应力的自定义蠕变模型,通过试验数据拟合获得了模型参数,所建模型能很好地描述延安地区重塑Q_3黄土的蠕变特性。  相似文献   

15.
王强  魏世强  刘保峰 《土壤学报》2005,42(4):600-608
研究了Fe2O3、MnO2或Al2O3固体吸附剂对胡敏酸和富里酸的吸附机制和影响因素。结果表明:相同pH下,Fe2O3、MnO2或Al2O3固体吸附剂对腐殖酸的吸附量随着腐殖酸(胡敏酸HA和富里酸FA)有机碳浓度的增加而增加;不同pH下,对HA的吸附量依照pH3·0>pH5·0>pH7·0的顺序递减。相同pH下,随着HA有机碳浓度的增加,三种固体吸附剂对HA的吸附百分率减小。相同pH下,三种固体吸附剂对FA的吸附百分率呈单峰形,随着酸度的降低,峰位向添加的有机碳低浓度处迁移。吸附量用Langumuir方程拟合能得到极显著相关的方程,在相同pH下,三种固体吸附剂吸附HA的最大吸附量Smax和吸附亲和力常数K小于FA,而标准自由能变ΔGmo却略大于FA;298·2K温度下,三种固体吸附剂吸附胡敏酸和富里酸的ΔGmo<0,表明在等温等压不做非体积功情况下吸附是自发进行的反应。  相似文献   

16.
17.
On the Tibetan Plateau, the unique alpine climate factors of low air pressure, low CO2 partial pressure and low air temperature have significant but non-explicit influences on the photosynthetic capacity of plants. To evaluate these influences, we measured the net photosynthetic rates for spring hulless barley leaves at two altitudes of 3688 m (the low altitude) and 4333 m (the high altitude), respectively. Two photosynthetic parameters—Vcmax, the maximum rate of Rubisco carboxylase activity, and Jmax, the maximum rate of photosynthetic electron transport—were determined. The net photosynthetic rate and the photosynthetic parameters Vcmax and Jmax were higher for leaves from plants grown at the high altitude than for those at the low altitude. Vcmax and Jmax were approximately 24% and 22% greater, respectively, for leaves from plants grown at the high altitude. The CO2 and air temperature at the high altitude were lower than those at the low altitude. As a consequence, plants exposed to lower CO2 partial pressure and lower air temperature have a higher photosynthetic capacity on the Tibetan Plateau. The optimal temperatures for Vcmax and Jmax were approximately 6.5% and 3.5% higher, respectively, in leaves from plants grown at the high altitude than those grown at the low altitude, and the ratio of Jmax to Vcmax was 12.7% lower at the low altitude. Simulation analyses revealed that the photosynthetic capacities of plants decreased after long-term increases in CO2 partial pressure and temperature associated with global climate change on the Tibetan Plateau.  相似文献   

18.
何娴  徐仁扣 《土壤》2022,54(5):1016-1023
选择稻草、玉米秸秆和油菜秸秆作为制备生物质炭的原料,分别用H2O2和HNO3/H2SO4对生物质炭进行改性处理,以未改性的生物质炭和HCl处理的生物质炭作为对照。按土重3%的比例向采自安徽郎溪的酸性水稻土中添加上述生物质炭,在经历一个干湿交替周期后,进行Cd(Ⅱ)吸附/解吸实验,研究添加生物质炭对水稻土吸附Cd(Ⅱ)的影响及其机制。结果表明,两种改性方法均有效增加了生物质炭表面的质子结合位点数,且HNO3/H2SO4改性对生物质炭表面羧基官能团的扩增效果更显著。官能团的增加使得添加了HNO3/H2SO4改性生物质炭的水稻土对Cd(Ⅱ)的专性吸附能力显著增强。因此,添加HNO3/H2SO4改性生物质炭可以作为酸性水稻土吸附固定重金属Cd的一种新型方法。  相似文献   

19.
升高CO2浓度能够促进作物的光合作用,提高作物的生物量和产量,但关于CO2与NH+4/NO-3比及其交互作用对作物影响的研究较少,为探索番茄幼苗生长发育对CO2浓度升高的响应是否对NH+4/NO-3配比有较强的依赖关系,本试验在营养液栽培条件下,以番茄(Lycopersicun esculentum Mill)为试材,研究正常大气CO2浓度(360 μL/L)和倍增CO2浓度(720 μL/L)与不同NH+4/NO-3配比的交互作用对番茄幼苗生长的影响。结果表明:CO2浓度升高提高了低NH+4/NO-3比例处理中番茄叶片的光合速率和水分利用率,提高幅度随NH+4/NO-3比例的降低而增强,光合速率增强最大达55%。在同一CO2浓度处理下净光合速率与水分利用率均随NH+4/NO-3比例的增加而显著降低。这说明CO2浓度升高对番茄幼苗生长发育的促进作用随NH+4/NO-3比例的降低而提高,但并没有减弱全NH+4-N处理中番茄幼苗的受毒害作用。综上所述,CO2浓度升高能提高植物生产的节水能力和水分生产力;水培条件下,NO-3-N是最适合番茄幼苗生长发育的氮源,其它NH+4/NO-3比例对番茄幼苗的生长发育有一定的抑制作用,仅以NH+4-N作氮源则番茄幼苗很难生长。  相似文献   

20.
The influence of NH4+ on microbial CH4 oxidation is still poorly understood. Therefore, the influence of NH4Cl and (NH4)2SO4 on CH4 oxidation was studied in soils at the different stages of the induction of enhanced methanotrophic activity. After a brief peak in the methanotrophic activity, a steady state was observed in which NH4+ inhibited CH4 oxidation at low CH4 concentrations, and stimulated CH4 oxidation at high concentrations. Chloride did not strongly inhibit CH4 oxidation during this phase. During a second phase methanotrophic activity increased again. Ammonium no longer stimulated CH4 oxidation, and Cl became an important source of uncompetitive inhibition. It was hypothesized that type I methanotrophs dominated during the first, soil-N-dependent phase while N2-fixing type II methanotrophs dominated the second, soil-N-independent phase.  相似文献   

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