植物根系分泌物生态效应及其影响因素研究综述

植物根系分泌物的形成是植物体代谢过程中重要的生理现象,为“植物-土壤”体系物质周转的重要环节.研究植物根系分泌物对于了解陆地生态系统质能过程、碳氮收支平衡及提高生态系统的初级生产具有重要意义.本文从植物根系分泌物对植物生理性状、土壤微生物、土壤物质周转及有机污染物降解影响等4个方面对植物根系分泌物的生态效应进行综述,并从重金属含量、营养元素水平、土壤水分和光热条件、物种基因型、土壤微生物状况和外源有机污染物添加的角度综述了影响植物根系分泌物的因素,旨在对植物根系分泌物的生态效应和影响因素进行总结,并根据目前的研究现状,从研究对象、研究方法和效应评估方面进行了展望.     

根系分泌物及其在植物修复中的作用

 近年来环境污染日益严重,污染物在土壤植物中的行为引起了人们的高度关注。利用植物去除土壤水体等介质中污染物的植物修复是近10年来兴起的一项安全、廉价的技术,已成为污染生态学和环境生态学的研究热点,它通过植物吸收、根滤、稳定、挥发等方式清除环境中的重金属和有机污染物。国内外有关植物修复的研究报道和概述很多, 但对植物根系分泌物在植物修复中所起的作用及其机理少有述评。 本文从根系分泌物对土壤重金属和土壤有机污染物的去除作用出发,对根系分泌物的种类、数量及其在去除环境污染物中的作用机理和功能地位进行了总结,并借助研究事例对影响植物根系分泌的内外因子,如植物种类、营养胁迫、重金属胁迫、根际环境的理化性质、土壤微生物及其它环境因子进行了讨论。概言之,根系分泌物在修复污染土壤中的重金属途径是多种多样的,主要是通过调节根际pH值、与重金属形成螯合物、络合反应、沉淀、提高土壤微生物数量和活性来改变重金属在根际中的存在形态以及提高重金属的生物有效性,从而减轻它对环境的危害。在清除有机污染物时,根系分泌物中的酶可以对有机污染物进行直接降解,根系分泌物影响下的微生物也可以对有机污染物进行间接降解,且被认为是主要的降解途径。根系分泌物在植物修复过程中确实起着某些重要作用,今后应将这方面的研究重点放在某些特异性根系分泌物植物,尤其是某些重金属超富集植物资源的寻找、筛选上,通过室内实验和野外研究确定其根系分泌物对清除重金属和有机污染物的效率,证实超富集植物根系分泌物的特异性与污染物超富集的内在联系,找到污染土壤生态恢复和治理的有效方法并加以推广应用,如针对性地在被污染地大面积种植此类具特异性根分泌物植物,并辅以营林措施如修剪等,加快生物修复进程,提高修复效率。植物根系分泌物在植物修复过程中所具有的重要生态意义和可能应用前景,为污染生态学和化学生态学之间的联合研究开拓了全新的领域,今后将取得新的突破和重要进展。     

外源有机质对土壤中菲的增强固定作用

从吸附、解吸、可萃取态残留变化3个方面,研究了外源有机质对粘壤土、砂粉土和粉壤土中菲的增强固定作用.外源有机质为有机商品肥和泥炭.结果表明,施加外源有机质后,供试土壤对菲的吸附等温线仍呈线性,分配作用为土壤吸附菲的主导机制.有机商品肥或泥炭能显著促进供试土样对菲的吸附.施加同量的外源有机质,土壤吸附菲的Kd值的增加幅度与土壤有机碳含量（foc）成正比,表明土壤的foc越大,外源有机质对菲吸附的促进效果越好.解吸实验表明,施加外源有机商品肥或泥炭能够抑制土壤中菲的解吸,解吸量显著低于原土.经64d培养,施加外源有机质的3种土壤中的可萃取态残留菲含量降低;由于泥炭的有机质含量高于有机商品肥,施加泥炭的土样中可萃取态残留菲的降幅更大;原土的foc越高,外源有机质对菲可萃取性的抑制效果越明显.可见,施加外源有机质可增强土壤中菲的吸附固定、抑制其解吸、并降低其可萃取态残留.     

模拟根系分泌物C:N化学计量特征对川西亚高山森林土壤碳动态和微生物群落结构的影响

目前有关森林根系分泌物及其诱导的土壤生态学效应研究主要关注根系碳(C)源输入, 而极少关注根系分泌物氮(N)源输入及其伴随的C:N化学计量特征对土壤过程和功能的影响, 极大地限制了我们对森林根系-土壤-微生物互作机制的深入认识。该研究以川西亚高山天然林和云杉(Picea asperata)人工林土壤为对象, 模拟配制不同C:N化学计量特征(只有N、C:N = 10、C:N = 50、C:N = 100和只有C处理)的根系分泌物溶液进行人工添加试验, 以探究根系分泌物化学计量特征对两种林分土壤碳动态及其微生物群落结构的影响差异。结果表明: 模拟根系分泌物C添加总体促进了两种林分土壤有机质分解激发效应而降低了土壤总碳(TC)含量, 而N添加在一定程度上缓和了两种林分土壤TC含量的降低幅度, 且C添加导致天然林土壤TC含量的降低幅度明显低于土壤N有效性更低的人工林。几种根系分泌物添加处理对两种林分土壤活性和惰性碳库的影响无明显规律。另外, 根系分泌物C添加总体降低了天然林土壤微生物总磷脂脂肪酸(PLFA)含量和细菌、放线菌、真菌PLFA含量, 而总体增加人工林土壤微生物PLFA总量和细菌、放线菌、真菌PLFA含量, 并诱导两种林分土壤微生物群落结构(细菌:真菌相对丰度)也发生了各自不同的变化。上述结果表明森林根系分泌物N源输入和土壤N有效性共同调控根系C源输入对土壤有机质分解激发效应的方向和幅度。研究结果为深入揭示典型森林根系分泌物化学计量特征对土壤生物化学循环过程的调控机制提供了一定的理论依据。     

Effects of simulated exudate C:N stoichiometry on dynamics of carbon and microbial community composition in a subalpine coniferous forest of western Sichuan,China

 目前有关森林根系分泌物及其诱导的土壤生态学效应研究主要关注根系碳(C)源输入, 而极少关注根系分泌物氮(N)源输入及其伴随的C:N化学计量特征对土壤过程和功能的影响, 极大地限制了我们对森林根系-土壤-微生物互作机制的深入认识。该研究以川西亚高山天然林和云杉(Picea asperata)人工林土壤为对象, 模拟配制不同C:N化学计量特征(只有N、C:N = 10、C:N = 50、C:N = 100和只有C处理)的根系分泌物溶液进行人工添加试验, 以探究根系分泌物化学计量特征对两种林分土壤碳动态及其微生物群落结构的影响差异。结果表明: 模拟根系分泌物C添加总体促进了两种林分土壤有机质分解激发效应而降低了土壤总碳(TC)含量, 而N添加在一定程度上缓和了两种林分土壤TC含量的降低幅度, 且C添加导致天然林土壤TC含量的降低幅度明显低于土壤N有效性更低的人工林。几种根系分泌物添加处理对两种林分土壤活性和惰性碳库的影响无明显规律。另外, 根系分泌物C添加总体降低了天然林土壤微生物总磷脂脂肪酸(PLFA)含量和细菌、放线菌、真菌PLFA含量, 而总体增加人工林土壤微生物PLFA总量和细菌、放线菌、真菌PLFA含量, 并诱导两种林分土壤微生物群落结构(细菌:真菌相对丰度)也发生了各自不同的变化。上述结果表明森林根系分泌物N源输入和土壤N有效性共同调控根系C源输入对土壤有机质分解激发效应的方向和幅度。研究结果为深入揭示典型森林根系分泌物化学计量特征对土壤生物化学循环过程的调控机制提供了一定的理论依据。     

土壤活性有机质及其与土壤质量的关系

活性有机质是土壤的重要组成部分 ,主要包括溶解性有机碳、微生物生物量、轻组有机质。它在土壤中具有重要作用 :(1)可以表征土壤物质循环特征、评价土壤质量 ,可以作为土壤潜在生产力以及由土壤管理措施引起土壤有机质变化的早期指标 ;(2 )在养分周转中起重要作用 ,是植物的养分库 ,可以提供植物所需要的养分如氮、磷、硫等 ;(3)能稳定土壤结构 ,对维持团粒结构稳定性有重要作用。从土壤养分、土壤物理、化学性质方面讨论了活性有机质与土壤质量的关系。土壤中的溶解性有机碳、微生物生物量碳氮含量与土壤有机碳、全氮和碱解氮等物质的含量呈正相关。活性有机质受土壤质地、含水量、温度等因素影响 ,与土壤酸碱度、阳离子交换量等也有关。土壤微生物生物量碳和微生物量 C/有机碳比与土壤粘粒、粉粒含量呈正相关、与砂粒含量呈负相关     

外源有机质对土壤中菲的增强固定作用

从吸附、解吸、可萃取态残留变化3个方面,研究了外源有机质对粘壤土、砂粉土和粉壤土中菲的增强固定作用.外源有机质为有机商品肥和泥炭.结果表明,施加外源有机质后,供试土壤对菲的吸附等温线仍呈线性,分配作用为土壤吸附菲的主导机制.有机商品肥或泥炭能显著促进供试土样对菲的吸附.施加同量的外源有机质,土壤吸附菲的K_d值的增加幅度与土壤有机碳含量(f_oc)成正比,表明土壤的f_oc越大,外源有机质对菲吸附的促进效果越好.解吸实验表明,施加外源有机商品肥或泥炭能够抑制土壤中菲的解吸,解吸量显著低于原土.经64 d培养,施加外源有机质的3种土壤中的可萃取态残留菲含量降低;由于泥炭的有机质含量高于有机商品肥,施加泥炭的土样中可萃取态残留菲的降幅更大;原土的f_oc越高,外源有机质对菲可萃取性的抑制效果越明显.可见,施加外源有机质可增强土壤中菲的吸附固定、抑制其解吸、并降低其可萃取态残留.     

氮添加对森林植物磷含量的影响及其机制

氮沉降对森林生态系统磷循环产生了不可忽视的影响,尤其是加剧了植物生长的磷限制,从而使得氮沉降背景下植物磷含量变化备受关注。该文综述了氮添加对森林植物磷含量的影响,认为氮添加通过促进土壤磷酸酶活性进而提高土壤有效磷含量,有利于植物的磷吸收并增加植物磷含量。同时,森林植物磷含量对氮添加的响应还受物种、生活型以及施氮时间长短等因素的影响。基于森林植物磷含量对氮添加响应的差异性,该文进一步探讨氮富集背景下森林植物磷含量变化的可能机制:1)外源氮输入通过改变土壤中有效磷含量从而对植物磷的来源产生影响; 2)通过影响植物的根系分泌物、菌根共生和根系形态结构等进而影响植物的磷吸收能力;3)通过影响植物的磷养分再分配、磷养分重吸收对植物磷利用效率产生影响。综上所述,外源氮输入使植物磷含量发生改变,首要原因是土壤有效磷含量的改变,其次是植物磷吸收能力和磷利用效率的改变起调控作用。     

氮添加对森林植物磷含量的影响及其机制

氮沉降对森林生态系统磷循环产生了不可忽视的影响, 尤其是加剧了植物生长的磷限制, 从而使得氮沉降背景下植物磷含量变化备受关注。该文综述了氮添加对森林植物磷含量的影响, 认为氮添加通过促进土壤磷酸酶活性进而提高土壤有效磷含量, 有利于植物的磷吸收并增加植物磷含量。同时, 森林植物磷含量对氮添加的响应还受物种、生活型以及施氮时间长短等因素的影响。基于森林植物磷含量对氮添加响应的差异性, 该文进一步探讨氮富集背景下森林植物磷含量变化的可能机制: 1)外源氮输入通过改变土壤中有效磷含量从而对植物磷的来源产生影响; 2)通过影响植物的根系分泌物、菌根共生和根系形态结构等进而影响植物的磷吸收能力; 3)通过影响植物的磷养分再分配、磷养分重吸收对植物磷利用效率产生影响。综上所述, 外源氮输入使植物磷含量发生改变, 首要原因是土壤有效磷含量的改变, 其次是植物磷吸收能力和磷利用效率的改变起调控作用。     

根系分泌物C∶N对刺槐林地土壤理化特征和土壤呼吸的影响

为探究根系分泌物C∶N对土壤养分循环及微生物活性的影响,本研究以黄土高原人工刺槐林为对象,在生境条件基本一致的15、25、35、45 a刺槐林地取原位土壤,通过模拟不同C∶N的根系分泌物(只添加N、C∶N=10、C∶N=50、C∶N=100和只添加C)添加至土壤,以去离子水作为对照,分析根系分泌物C∶N对土壤碳、氮、磷、pH值等理化特征和土壤呼吸的影响。结果表明: 1)有机碳含量与根系分泌物C∶N呈正相关,根系分泌物C∶N=10时土壤有机碳(SOC)分解较快,高根系分泌物C∶N(C∶N=100)能延缓SOC分解,而只添加C处理对SOC无显著影响。2)不同C∶N根系分泌物处理对全氮的影响不明显,碳添加能促进微生物对铵态氮的吸收,氮添加能促进铵态氮的硝化,随着根系分泌物C∶N增加,土壤中铵态氮含量下降。3)氮添加会导致土壤pH值下降,增加土壤全磷含量。4)刺槐林地土壤呼吸值与根系分泌物C∶N呈正相关,随着C∶N增加,根系分泌物对25和35 a人工刺槐林土壤呼吸的促进作用更显著。综上,根系分泌物C∶N值越高,对人工刺槐林土壤呼吸的促进作用越显著。研究结果进一步加深了对森林根系-土壤-微生物互作过程的认识。     

稻田甲烷排放模型研究——模型及其修正

在过去十多年内 ,关于稻田甲烷排放的模拟已经进行了不少有益的探索并且开发出了数个有关的模型。模型的成功研制是准确定量估计不同区域范围内稻田甲烷排放的前提。以往大部分模型由于模拟精度不高 ,或者是其要求太多的输入参数 ,因而限制了它在大尺度范围内的广泛应用。在一个比较成熟的模型基础上 ,进行了必要的修正与扩充。增加了稻田甲烷通过气泡方式排放的模拟模块 ,并修正了原模型中关于土壤氧化还原电位变化的模拟 ,使之能适应于多种稻田水管理方式。新修正的模型 (CH4 MOD)不仅保留了原模型输入参数较少和易于获得的优点 ,而且能适应多种水稻耕作方式 ,这为进一步利用模型技术准确估计大尺度区域稻田甲烷排放提供了一种新的科学方法     

Agronomic aspects of wetland rice cultivation and associated methane emissions

Wetland rice cultivation is one of the major sources of atmospheric methane (CH₄). Global rice production may increase by 65% between 1990 and 2025, causing an increase of methane emissions from a 92 Tg CH₄ y^–1 now to 131 Tg in 2025.Methane production depends strongly on the ratio oxidizing: reducing capacity of the soil. It can be influenced by e.g. addition of sulphate, which inhibits methanogenesis. The type and application mode of mineral fertilizers may also affect methane emissions. Addition of organic matter in the form of compost or straw causes an increase of methane emissions, but methane production is lower for materials with a low C/N ratio.High percolation rates in wetland rice soils and occasional drying up of the soil during the cultivation period depresses methane release. Water management practices aimed at reducing emissions are only feasible during specific periods in the rice growing season in flat lowland irrigated areas with high security of water availability and good control of the water supply. Intermittent drying of soils may not be possible on terraced rice lands.Assuming a 10 to 30% reduction in emission rates per unit harvested area, the global emission may amount to 93 Tg CH₄ y^– in 2025. A reduction of global emissions seems very difficult. To develop techniques for reducing CH₄ emissions from wetland rice fields, research is required concerning interactions between soil chemical and physical properties, and soil, water and crop management and methanogenesis. Such techniques should not adversely affect rice yields.     

The rate of permafrost carbon release under aerobic and anaerobic conditions and its potential effects on climate

Recent observations suggest that permafrost thaw may create two completely different soil environments: aerobic in relatively well‐drained uplands and anaerobic in poorly drained wetlands. The soil oxygen availability will dictate the rate of permafrost carbon release as carbon dioxide (CO₂) and as methane (CH₄), and the overall effects of these emitted greenhouse gases on climate. The objective of this study was to quantify CO₂ and CH₄ release over a 500‐day period from permafrost soil under aerobic and anaerobic conditions in the laboratory and to compare the potential effects of these emissions on future climate by estimating their relative climate forcing. We used permafrost soils collected from Alaska and Siberia with varying organic matter characteristics and simultaneously incubated them under aerobic and anaerobic conditions to determine rates of CO₂ and CH₄ production. Over 500 days of soil incubation at 15 °C, we observed that carbon released under aerobic conditions was 3.9–10.0 times greater than anaerobic conditions. When scaled by greenhouse warming potential to account for differences between CO₂ and CH₄, relative climate forcing ranged between 1.5 and 7.1. Carbon release in organic soils was nearly 20 times greater than mineral soils on a per gram soil basis, but when compared on a per gram carbon basis, deep permafrost mineral soils showed carbon release rates similar to organic soils for some soil types. This suggests that permafrost carbon may be very labile, but that there are significant differences across soil types depending on the processes that controlled initial permafrost carbon accumulation within a particular landscape. Overall, our study showed that, independent of soil type, permafrost carbon in a relatively aerobic upland ecosystems may have a greater effect on climate when compared with a similar amount of permafrost carbon thawing in an anaerobic environment, despite the release of CH₄ that occurs in anaerobic conditions.     

Fluxes of N2O,CH4 and CO2 on afforested boreal agricultural soils

After drainage of natural boreal peatlands, the decomposition of organic matter increases and peat soil may turn into a net source of CO₂ and N₂O, whereas CH₄ emission is known to decrease. Afforestation is a potential mitigation strategy to reduce greenhouse gas emission from organic agricultural soils. A static chamber technique was used to evaluate the fluxes of CH₄, N₂O and CO₂ from three boreal organic agricultural soils in western Finland, afforested 1, 6 or 23 years before this study. The mean emissions of CH₄ and N₂O during the growing seasons did not correlate with the age of the tree stand. All sites were sources of N₂O. The highest daily N₂O emission during the growing season, measured in the oldest site, was as high as 29 mg N₂O m^–2d^–1. In general, organic agricultural soils are sinks for methane. Here, the oldest site acted as a small sink for methane, whereas the two youngest afforested organic soils were sources for methane with maximum emission rates (up to 154 mg m^–2d^–1) similar to those reported for minerogenous natural peatlands. Soil respiration rates decreased with the age of the forest. The high soil respiration in the younger sites, probably resulted from the high biomass production of herbs, could create soil anaerobiosis and increase methane production. Our results show that afforestation of agricultural peat soils does not abruptly terminate the N₂O emissions during the first two decades, and afforestation can even enhance methane emission for a few years. The carbon accumulation in the developing tree stand can partly compensate the carbon loss from soil.     

Impact of root exudates of different cultivars and plant development stages of rice (Oryza sativa L.) on methane production in a paddy soil

The impact of root exudates, collected from five rice cultivars, on methane (CH₄) production was studied in a paddy soil under anaerobic conditions. Root exudates of the cultivars Dular, IR72 and IR65598 collected at four growth stages and of B40 and IR65600 collected at two growth stages showed that (a) CH₄ production was commenced rapidly within 2 h upon exudate addition and reached a maximum within a day of addition, and (b) 7-d incubation periods were sufficient to study exudate-induced CH₄ production potentials. Among different cultivars, high C releases from roots, increased the methanogenic source strength of the soil, which finally controlled CH₄ production. The relationship of the amount of CH₄ produced was stronger for the amount of total organic C (r = 0.920) than for the amount of organic acids (r = 0.868) added through exudates. Apparently, CH₄ production and CH₄ emission are more closely related to the release pattern of root exudate-C than to its individual components. The proportion of exudate-C converted to CH₄ ranged between 61 and 83% and remained unaffected by cultivars and growth stages suggesting that the majority of exudate-C served as a methanogenic substrate in the anoxic rice soils. These observations indicate that the use of high-yielding cultivars with lowest excretion (for example IR65598, IR65600) would result in lowest exudate-induced CH₄ production. Therefore, cultivar choice could greatly influence regional and global CH₄ emissions and screening/selection of exiting rice cultivars, and/or breeding new cultivars with low exudation rates could offer an important methane mitigation option as long as yields are not compromised.     

Water salinity and inundation control soil carbon decomposition during salt marsh restoration: An incubation experiment

Coastal wetlands are a significant carbon (C) sink since they store carbon in anoxic soils. This ecosystem service is impacted by hydrologic alteration and management of these coastal habitats. Efforts to restore tidal flow to former salt marshes have increased in recent decades and are generally associated with alteration of water inundation levels and salinity. This study examined the effect of water level and salinity changes on soil organic matter decomposition during a 60‐day incubation period. Intact soil cores from impounded fresh water marsh and salt marsh were incubated after addition of either sea water or fresh water under flooded and drained water levels. Elevating fresh water marsh salinity to 6 to 9 ppt enhanced CO₂ emission by 50%?80% and most typically decreased CH₄ emissions, whereas, decreasing the salinity from 26 ppt to 19 ppt in salt marsh soils had no effect on CO₂ or CH₄ fluxes. The effect from altering water levels was more pronounced with drained soil cores emitting ~10‐fold more CO₂ than the flooded treatment in both marsh sediments. Draining soil cores also increased dissolved organic carbon (DOC) concentrations. Stable carbon isotope analysis of CO₂ generated during the incubations of fresh water marsh cores in drained soils demonstrates that relict peat OC that accumulated when the marsh was saline was preferentially oxidized when sea water was introduced. This study suggests that restoration of tidal flow that raises the water level from drained conditions would decrease aerobic decomposition and enhance C sequestration. It is also possible that the restoration would increase soil C decomposition of deeper deposits by anaerobic oxidation, however this impact would be minimal compared to lower emissions expected due to the return of flooding conditions.     

Soil microorganisms as controllers of atmospheric trace gases (H2, CO, CH4, OCS, N2O, and NO).

Production and consumption processes in soils contribute to the global cycles of many trace gases (CH4, CO, OCS, H2, N2O, and NO) that are relevant for atmospheric chemistry and climate. Soil microbial processes contribute substantially to the budgets of atmospheric trace gases. The flux of trace gases between soil and atmosphere is usually the result of simultaneously operating production and consumption processes in soil: The relevant processes are not yet proven with absolute certainty, but the following are likely for trace gas consumption: H2 oxidation by abiontic soil enzymes; CO cooxidation by the ammonium monooxygenase of nitrifying bacteria; CH4 oxidation by unknown methanotrophic bacteria that utilize CH4 for growth; OCS hydrolysis by bacteria containing carbonic anhydrase; N2O reduction to N2 by denitrifying bacteria; NO consumption by either reduction to N2O in denitrifiers or oxidation to nitrate in heterotrophic bacteria. Wetland soils, in contrast to upland soils are generally anoxic and thus support the production of trace gases (H2, CO, CH4, N2O, and NO) by anaerobic bacteria such as fermenters, methanogens, acetogens, sulfate reducers, and denitrifiers. Methane is the dominant gaseous product of anaerobic degradation of organic matter and is released into the atmosphere, whereas the other trace gases are only intermediates, which are mostly cycled within the anoxic habitat. A significant percentage of the produced methane is oxidized by methanotrophic bacteria at anoxic-oxic interfaces such as the soil surface and the root surface of aquatic plants that serve as conduits for O2 transport into and CH4 transport out of the wetland soils. The dominant production processes in upland soils are different from those in wetland soils and include H2 production by biological N2 fixation, CO production by chemical decomposition of soil organic matter, and NO and N2O production by nitrification and denitrification. The processes responsible for CH4 production in upland soils are completely unclear, as are the OCS production processes in general. A problem for future research is the attribution of trace gas metabolic processes not only to functional groups of microorganisms but also to particular taxa. Thus, it is completely unclear how important microbial diversity is for the control of trace gas flux at the ecosystem level. However, different microbial communities may be part of the reason for differences in trace gas metabolism, e.g., effects of nitrogen fertilizers on CH4 uptake by soil; decrease of CH4 production with decreasing temperature; or different rates and modes of NO and N2O production in different soils and under different conditions.     

Methanogenic communities in permafrost-affected soils of the Laptev Sea coast, Siberian Arctic, characterized by 16S rRNA gene fingerprints

Permafrost environments in the Arctic are characterized by extreme environmental conditions that demand a specific resistance from microorganisms to enable them to survive. In order to understand the carbon dynamics in the climate-sensitive Arctic permafrost environments, the activity and diversity of methanogenic communities were studied in three different permafrost soils of the Siberian Laptev Sea coast. The effect of temperature and the availability of methanogenic substrates on CH4 production was analysed. In addition, the diversity of methanogens was analysed by PCR with specific methanogenic primers and by denaturing gradient gel electrophoresis (DGGE) followed by sequencing of DGGE bands reamplified from the gel. Our results demonstrated methanogenesis with a distinct vertical profile in each investigated permafrost soil. The soils on Samoylov Island showed at least two optima of CH4 production activity, which indicated a shift in the methanogenic community from mesophilic to psychrotolerant methanogens with increasing soil depth. Furthermore, it was shown that CH4 production in permafrost soils is substrate-limited, although these soils are characterized by the accumulation of organic matter. Sequence analyses revealed a distinct diversity of methanogenic archaea affiliated to Methanomicrobiaceae, Methanosarcinaceae and Methanosaetaceae. However, a relationship between the activity and diversity of methanogens in permafrost soils could not be shown.     

A semi-empirical model of methane emission from flooded rice paddy soils

Reliable regional or global estimates of methane emissions from flooded rice paddy soils depend on an examination of methodologies by which the current high variability in the estimates might be reduced. One potential way to do this is the development of predictive models. With an understanding of the processes of methane production, oxidation and emission, a semi-empirical model, focused on the contributions of rice plants to the processes and also the influence of environmental factors, was developed to predict methane emission from flooded rice fields. A simplified version of the model was also derived to predict methane emission in a more practical manner. In this study, it was hypothesized that methanogenic substrates are primarily derived from rice plants and added organic matter. Rates of methane production in flooded rice soils are determined by the availability of methanogenic substrates and the influence of environmental factors. Rice growth and development control the fraction of methane emitted. The amount of methane transported from the soil to the atmosphere is determined by the rates of production and the emitted fraction. Model validation against observations from single rice growing seasons in Texas, USA demonstrated that the seasonal variation of methane emission is regulated by rice growth and development. A further validation of the model against measurements from irrigated rice paddy soils in various regions of the world, including Italy, China, Indonesia, Philippines and the United States, suggests that methane emission can be predicted from rice net productivity, cultivar character, soil texture and temperature, and organic matter amendments.     

多年冻土退化对湿地甲烷排放的影响研究进展

全球气候变暖导致北半球大部分多年冻土区的冻土已经开始退化。多年冻土退化对冻土区湿地CH₄排放产生重要影响,可能直接决定冻土区湿地对全球气候变暖的反馈方式。综述了近年来多年冻土退化对湿地CH₄排放影响的研究。多年冻土退化导致的土壤活动层深度增加和植被类型由中生向湿生的转变都可能会大大增加冻土区湿地CH₄排放量,从而可能对全球气候变暖产生正反馈作用。但多年冻土退化导致的水文条件变化、土壤温度变化和微生物组成及活性变化对湿地CH₄排放的影响却存在一定的不确定性。多年冻土退化除了影响湿地CH₄排放量之外,还可能通过改变土壤冻融过程而影响湿地CH₄排放的季节分配模式。最后提出目前研究中存在的问题,并对未来研究方向进行了展望。