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1.
丛枝菌根对有机污染土壤的修复作用及机理   总被引:7,自引:0,他引:7  
丛枝菌根(AM)是丛枝菌根真菌(AMF)与植物根系相互作用的互惠共生体,能改良土壤结构,增强植物抗性.自然界中已知的AMF有170多种,分布广泛,且可与大多数植物共生.利用AM修复有机污染土壤正成为一个崭新的研究方向.本文综述了AM对多环芳烃、酞酸脂、石油和农药等一些典型有机污染物污染土壤的修复作用.AM修复有机污染土壤的机理主要包括:AMF代谢有机污染物;AM分泌酶,降解污染物;AM影响根系分泌作用,并促进根际微生物对有机污染物的降解;AMF宿主植物吸收积累污染物.AM修复研究中,高效AMF的筛选、复合菌种效应、土壤老化、AM作用下植物对有机污染物的吸收积累等几方面仍有待于深入研究.  相似文献   

2.
嗜热菌对有机污染物的降解及其应用研究进展   总被引:2,自引:0,他引:2  
有机污染物造成的环境问题日趋严重,嗜热菌具有高效降解环境有机污染物的潜力.嗜热菌在高温条件下降解有机污染物,代谢速度快,嗜温杂菌的竞争减少,同时高温环境下一些难降解有机物的溶解度和生物可利用性大大提高,有机污染物可得到快速、彻底降解.因此,嗜热菌对有机废水生物处理及有机物污染场地生物修复等意义重大.本文从嗜热菌降解有机污染物的特点、温度的影响、降解途径、降解酶及其编码基因及工程应用等角度,介绍了嗜热菌降解有机污染物的研究进展,并对嗜热菌降解有机污染物的机理、菌种资源储备、技术策略及应用研发等研究方向进行了展望.  相似文献   

3.
有机污染物在表层土壤中光降解的研究进展   总被引:5,自引:0,他引:5  
土壤是承载有机污染物的重要介质,而光降解是降解土壤表层有机污染物的一种非常重要的非生物转化途径。研究土壤表层有机物的光降解对认识污染物土壤环境行为有非常重要的意义。20世纪90年代以来对土壤中有机污染物的光降解研究有了大量报道。本文阐述了土壤组成和质地、土壤湿度、土壤pH值和土壤厚度等因素对光解影响的研究现状;介绍了目前研究土壤光降解所采用的研究方法:土壤表层直接光解、土壤悬浮液光解、溶剂萃取与光降解联合处理,及其研究土壤光降解应用的动力模型;对不同农药和其它有机污染物在土壤中的光降解研究进行了综述,并对今后的研究作了展望。  相似文献   

4.
高分子量多环芳烃( HMW PAHs)分子结构复杂,疏水性强,是环境中广泛存在的难降解的有机污染物.微生物降解是去除HMW PAHs的主要途径.本文介绍了PAHs降解菌株的种类和降解机理,以及不同环境因子(营养元素、pH值、土壤结构、通气状况和复合污染)对HMW PAHs降解的影响,提出HMW PAHs污染土壤的进一步研究的方向与重点,旨在为HMW PAHs污染修复研究和微生物降解机理研究提供参考.  相似文献   

5.
有机污染物在土壤中老化行为的研究进展   总被引:2,自引:0,他引:2  
赵青  李培军 《生态学杂志》2008,27(3):476-479
有机污染物在土壤中的老化行为是目前有机污染研究的一个热点问题.通过对其机理的研究,可以达到调控污染物的目的.本文介绍了有机污染物在土壤中的老化行为和国内外研究现状,指出老化的实质包括有机污染物在土壤中的慢吸附和锁定,总结了土壤性质、化合物性质和环境因素对老化的影响,同时介绍了老化的评价方法,并在此基础上提出了目前研究有机物在土壤老化过程中所存在的问题,并对老化行为的未来研究方向进行了展望.  相似文献   

6.
微生物菌剂在难降解有机污染治理的研究进展   总被引:2,自引:0,他引:2       下载免费PDF全文
大量的难降解有机污染物被排放到环境中,因其蓄积性、持久性和生物毒性,对人类健康和生态环境造成严重危害。近年来,利用微生物菌剂治理难降解有机污染物的研究已取得较好的进展。综述微生物菌剂在国内外的发展历程,介绍微生物菌剂制备中常用的固定化技术及载体材料,并分析总结微生物菌剂在酚类物质、多环芳烃和多氯联苯等有机污染物治理中的研究进展。在此基础上,提出治理难降解有机污染物的微生物菌剂研发所存在的主要问题及其展望。  相似文献   

7.
溶解性有机质对土壤中有机污染物环境行为的影响   总被引:32,自引:4,他引:28  
土壤中溶解性有机质(DOM)是生物活性和物理化学反应活性都很活跃的有机组分,主要通过疏水吸附、分配、氢键、电荷转移、共价键、范德华力等多种作用与有机污染物结合,提高溶液中有机污染物的溶解度,改变土壤中有机污染物的吸附-解吸、迁移-转化等环境行为.DOM对有机污染物的吸附-解吸、迁移-转化过程的影响有双重性:一方面,DOM与有机污染物在土壤表面的共吸附可增加土壤对有机污染物的吸附容量,促进有机污染物在土壤中的吸持;另一方面,DOM对有机污染物的增溶作用,有利于土壤中有机污染物的解吸,提高移动性.作为光敏剂,DOM能提高土壤中有机物的光解反应速率.在一定条件下,DOM也可影响土壤中有机污染物的水解过程.DOM对土壤中有机污染物环境行为的影响与DOM和有机污染物的性质及其相互作用的介质条件密切相关.  相似文献   

8.
转基因植物对有机污染物的吸收、转化和降解   总被引:7,自引:0,他引:7  
有机污染物是土壤、水体和大气环境的重要污染物.利用和加强植物修复作用是控制环境污染的有效途径.近年来,一些具有修复功能的外源基因被陆续引入到植物中,使转基因植物的生物修复能力大大增强.文章介绍了植物对污染环境中有机污染物,尤其是持久性有机污染物(POPs)的吸收、转化和降解作用,阐述了转基因植物用于被污染环境修复方面的研究进展和应用前景.  相似文献   

9.
根际圈在污染土壤修复中的作用与机理分析   总被引:71,自引:9,他引:62  
根际圈以植物根系为中心聚集了大量的生命物质及其分泌物,构成了极为独特的“生态修复单元”。本文叙述了根在根际圈污染土壤修复中的生理生态作用,富集、固定重金属,吸收、降解有机污染物等功能;菌根真菌对根际圈内重金属的吸收、屏障及螯合作用,对有机污染物的降解作用;根际圈内细菌对重金属的吸附与固定,对有机污染物的降解作用以及根际圈真菌和细菌的联合修复作用等,同时对可能存在的机理进行了分析,认为根际圈对污染土壤的修复作用是植物修复的重要组成部分和主要理论基础之一,并指出利用重金属超富集植物修复重金属污染土壤具有广阔的应用前景;筛选对水溶性有机污染物高吸收富集及其根 发泌能力强的特异植物,同时接种利于有机污染物降解的专性或非专性真菌和细菌可能会成为有机污染土壤植物修复研究的重要方向之一。  相似文献   

10.
沈阳市城郊土壤有机污染特征   总被引:1,自引:0,他引:1  
对沈阳市城郊土壤中35种有机污染物进行了检测,分析了土壤有机污染检出特征和空间分布特征.沈阳市城郊土壤共检出了15种有机污染物;苯并(a)芘、六氯苯、滴滴涕和六六六的变异系数均大于l,其污染物浓度局部富集程度高,含量起伏变化大,土壤有机污染呈现“一多三少”的现象,即全区检出有机污染物的采样点多,检出的有机污染物种类较少,有机污染物含量少,且无超标点.受土壤包气带岩性影响,城郊土壤垂向上有机污染规律明显.土壤区域有机污染分布特征与城市土地利用功能一致性较高.分析了各类有机污染物含量和分布特征的主要影响因素,对防治城市土壤污染,进而保障居民的食品安全和饮水安全具有重要意义.  相似文献   

11.
土壤团聚体固碳的研究方法   总被引:5,自引:0,他引:5  
增加土壤有机碳含量对维持土壤肥力和农业可持续发展,缓解温室气体增加和全球气候变化的影响具有重要意义.土壤团聚体是土壤的重要组成部分,影响着土壤的各种物理化学性质.土壤团聚体对土壤有机碳的物理保护是土壤碳固定的重要机制.本文综述了土壤团聚体对有机碳的固定作用,土壤团聚体固碳机制研究的经典方法和现代常规方法,并且针对研究中存在的问题探讨了今后的发展趋势.  相似文献   

12.
土壤铁矿物形态转化影响有机碳固定研究进展   总被引:1,自引:0,他引:1  
宋旭昕  刘同旭 《生态学报》2021,41(20):7928-7938
铁是地壳中丰度第四高的元素,其可通过多种方式影响土壤有机碳累积,尤其铁氧化物与土壤有机碳相互作用形成的稳定有机-矿物复合物,被认为是土壤可溶性有机碳长期固定的关键地球化学机制。促进土壤固定有机碳不仅可以提高土壤质量和肥力,还是应对全球气候变化的主要策略之一。然而,铁活跃的氧化还原反应和多样化的赋存形态,使其转化过程对土壤有机碳累积和稳定性的影响结果受到诸多生物和非生物因素调控。从不同角度,结合多学科的研究成果,综述了近年来国内外关于铁矿物形态转化影响土壤有机碳固定的相关研究,包括铁矿物形态转化过程、土壤有机碳固定机制、铁矿物形态转化影响土壤有机碳固定的机制及其主要影响因素(各种环境条件、自身的铁矿物性质、碳源质量等方面),强调铁在土壤有机碳固定过程中的重要作用。对铁固定土壤有机碳的相关研究提出了建议,为今后研究提供相关参考。  相似文献   

13.
Mechanisms of Carbon Sequestration in Soil Aggregates   总被引:12,自引:0,他引:12  
Soil and crop management practices have a profound impact on carbon (C) sequestration, but the mechanisms of interaction between soil structure and soil organic C (SOC) dynamics are not well understood. Understanding how an aggregate stores and protects SOC is essential to developing proper management practices to enhance SOC sequestration. The objectives of this article are to: (1) describe the importance of plants and soil functions on SOC sequestration, (2) review the mechanisms of SOC sequestration within aggregates under different vegetation and soil management practices, (3) explain methods of assessing distribution of SOC within aggregates, and (4) identify knowledge gaps with regards to SOC and soil structural dynamics. The quality and quantity of plant residues define the amount of organic matter and thus the SOC pool in aggregates. The nature of plant debris (C:N ratio, lignin content, and phenolic compound content) affects the rate of SOC sequestration. Mechanisms of interaction of aggregate dynamics with SOC are complex and embrace a range of spatial and temporal processes within macro- ( > 250 μ m e.c.d.) and microaggregates ( < 250 μ m e.c.d.). A relevant mechanism for SOC sequestration within aggregates is the confinement of plant debris in the core of the microaggregates. The C-rich young plant residues form and stabilize macroaggregates, whereas the old organic C is occluded in the microaggregates. Interactions of clay minerals with C rich humic compounds in correlation with clay mineralogy determine the protection and storage of SOC. Principal techniques used to assess the C distribution in aggregates include the determination of total organic C in different aggregate size fractions, isotopic methods to assess the turnover and storage of organic C in aggregates, and computed tomography and X-ray scattering to determine the internal porosity and inter-aggregate attributes. The literature is replete with studies on soil and crop management influences on total organic C and soil aggregation. However, research reports on the interactions of SOC within aggregates for C sequestration are scanty. Questions still remain on how SOC interacts physically and chemically with aggregates, and research is needed to understand the mechanisms responsible for the dynamics of aggregate formation and stability in relation to C sequestration.  相似文献   

14.
Biochar amendment is one of the most promising agricultural approaches to tackle climate change by enhancing soil carbon (C) sequestration. Microbial-mediated decomposition processes are fundamental for the fate and persistence of sequestered C in soil, but the underlying mechanisms are uncertain. Here, we synthesise 923 observations regarding the effects of biochar addition (over periods ranging from several weeks to several years) on soil C-degrading enzyme activities from 130 articles across five continents worldwide. Our results showed that biochar addition increased soil ligninase activity targeting complex phenolic macromolecules by 7.1%, but suppressed cellulase activity degrading simpler polysaccharides by 8.3%. These shifts in enzyme activities explained the most variation of changes in soil C sequestration across a wide range of climatic, edaphic and experimental conditions, with biochar-induced shift in ligninase:cellulase ratio correlating negatively with soil C sequestration. Specifically, short-term (<1 year) biochar addition significantly reduced cellulase activity by 4.6% and enhanced soil organic C sequestration by 87.5%, whereas no significant responses were observed for ligninase activity and ligninase:cellulase ratio. However, long-term (≥1 year) biochar addition significantly enhanced ligninase activity by 5.2% and ligninase:cellulase ratio by 36.1%, leading to a smaller increase in soil organic C sequestration (25.1%). These results suggest that shifts in enzyme activities increased ligninase:cellulase ratio with time after biochar addition, limiting long-term soil C sequestration with biochar addition. Our work provides novel evidence to explain the diminished soil C sequestration with long-term biochar addition and suggests that earlier studies may have overestimated soil C sequestration with biochar addition by failing to consider the physiological acclimation of soil microorganisms over time.  相似文献   

15.
Aliphatic hydrocarbons make up a substantial portion of organic contamination in the terrestrial environment. However, most studies have focussed on the fate and behaviour of aromatic contaminants in soil. Despite structural differences between aromatic and aliphatic hydrocarbons, both classes of contaminants are subject to physicochemical processes, which can affect the degree of loss, sequestration and interaction with soil microflora. Given the nature of hydrocarbon contamination of soils and the importance of bioremediation strategies, understanding the fate and behaviour of aliphatic hydrocarbons is imperative, particularly microbe-contaminant interactions. Biodegradation by microbes is the key removal process of hydrocarbons in soils, which is controlled by hydrocarbon physicochemistry, environmental conditions, bioavailability and the presence of catabolically active microbes. Therefore, the aims of this review are (i) to consider the physicochemical properties of aliphatic hydrocarbons and highlight mechanisms controlling their fate and behaviour in soil; (ii) to discuss the bioavailability and bioaccessibility of aliphatic hydrocarbons in soil, with particular attention being paid to biodegradation, and (iii) to briefly consider bioremediation techniques that may be applied to remove aliphatic hydrocarbons from soil.  相似文献   

16.
滨海盐沼湿地有着较高的碳沉积速率和固碳能力,在缓解全球变暖方面发挥着重要作用,而盐渍土壤是滨海盐沼湿地碳收支研究中最大的有机碳库,研究其碳沉积与埋藏对于理解滨海湿地碳收支有着重要的意义.本文从滨海盐沼湿地土壤有机碳的来源、土壤有机碳库与沉积速率、盐沼湿地有机碳的埋藏机制、全球变化与滨海盐沼湿地碳封存等几方面对滨海盐沼湿地有机碳沉积与埋藏的相关研究进行综述.今后研究应侧重:1)加强对控制滨海盐沼湿地碳储存变异的基本因素的进一步研究;2)对测量滨海盐沼湿地沉积物碳储量和沉积碳埋藏速率的方法进行标准化;3)对潮汐影响下滨海盐沼湿地碳与邻近生态系统之间的横向交换通量进行量化;4)探明全球变暖的影响和生产力的提高是否可以抵消因呼吸增强而造成的有机碳降解速率的升高.确定固碳速率变化驱动因子,理解气候变化和人类活动对碳埋藏的影响机制,有助于提升我国滨海盐沼湿地的固碳能力.  相似文献   

17.
滨海盐沼湿地是缓解全球变暖的有效蓝色碳汇, 但是近岸海域富营养化导致的大量氮输入对盐沼湿地稳定性和碳汇功能构成严重威胁。潮汐作用下大量氮输入对盐沼湿地植物光合碳输入、植物-土壤碳分配和土壤碳输出等碳循环关键过程产生深刻影响, 进而影响盐沼湿地碳汇功能评估的准确性。该文从植物光合固碳、植物-土壤系统碳分配、土壤有机碳分解、土壤可溶性有机碳释放、盐沼湿地土壤碳库5个方面综述了氮输入对盐沼湿地碳循环关键过程的影响。在此基础上, 针对当前研究的不足, 提出今后的研究中, 需要进一步探究氮输入对盐沼湿地植物光合固碳及碳分配过程的影响、盐沼湿地土壤有机碳分解的微生物机制、盐沼湿地土壤可溶性有机碳产生和横向流动的影响、以及氮类型对盐沼湿地土壤碳库的影响。以期为揭示氮输入对盐沼湿地碳汇形成过程与机制提供基础资料和理论依据, 为评估未来近岸海域水体富营养化影响下滨海盐沼湿地碳库的潜在变化提供新思路。  相似文献   

18.
Carbon sequestration potential in European croplands has been overestimated   总被引:5,自引:0,他引:5  
Yearly, per‐area carbon sequestration rates are used to estimate mitigation potentials by comparing types and areas of land management in 1990 and 2000 and projected to 2010, for the European Union (EU)‐15 and for four country‐level case studies for which data are available: UK, Sweden, Belgium and Finland. Because cropland area is decreasing in these countries (except for Belgium), and in most European countries there are no incentives in place to encourage soil carbon sequestration, carbon sequestration between 1990 and 2000 was small or negative in the EU‐15 and all case study countries. Belgium has a slightly higher estimate for carbon sequestration than the other countries examined. This is at odds with previous reports of decreasing soil organic carbon stocks in Flanders. For all countries except Belgium, carbon sequestration is predicted to be negligible or negative by 2010, based on extrapolated trends, and is small even in Belgium. The only trend in agriculture that may be enhancing carbon stocks on croplands at present is organic farming, and the magnitude of this effect is highly uncertain. Previous studies have focused on the potential for carbon sequestration and have shown quite significant potential. This study, which examines the sequestration likely to occur by 2010, suggests that the potential will not be realized. Without incentives for carbon sequestration in the future, cropland carbon sequestration under Article 3.4 of the Kyoto Protocol will not be an option in EU‐15.  相似文献   

19.
农田土壤固碳速率是评价土壤固碳效应和潜力的重要指标,精确估算区域农田土壤固碳速率对土壤地力及环境效应均具有重要意义.本研究选取黄淮海平原典型潮土区河南省封丘县为研究区域,按照土壤利用-土壤类型联合单元布点法,于2011年采集了70个耕层土样,测定了土壤有机碳含量、机械组成、容重、pH,并与全国第二次土壤普查(1981年)数据进行对比分析,结合地统计方法和GIS技术研究了该地区近30年农田土壤固碳速率的空间变异特征,利用显著性检验、回归分析、方差分析等方法定量分析了该区域农田土壤固碳速率的影响因素.结果表明: 近30年封丘县域土壤固碳速率平均值为0.33 t C·hm-2·a-1,变异系数为74%,属于中等变异性;土壤固碳速率的变化在东西方向上表现为西高东低、中部高南北低,呈片状分布,区域结构性因素是引起农田土壤固碳速率空间分布差异的主导因素,如土壤类型、机械组成、容重、pH,可解释空间变异的59.5%,其次是随机性因素,如秸秆还田量、施肥量,可解释空间变异的40.5%.  相似文献   

20.
Pan B  Huang P  Wu M  Wang Z  Wang P  Jiao X  Xing B 《Bioresource technology》2012,103(1):367-373
Sediment samples with high organic carbon contents (22.04% and 8.46%) were collected and thermally-treated using a method analogous to biochar production. The obtained thermally-treated sediments (TTSs) showed a much higher degree of carbon capture in comparison to biochar derived from common biomass, indicating potential use of TTSs in soil amendment and carbon sequestration. Their sorption with organic contaminants was also investigated using sulfamethoxazole (SMX) as a model sorbate. SMX sorption increased greatly with pyrolytic temperature. Desorption ratio of the adsorbed SMX in TTSs generally decreased with increased pyrolytic temperature and with decreased solid-phase concentrations. The thermodynamic analysis showed that the higher entropy increase (positive ΔS) was well related with the decreased desorption ratio with increased solid-phase concentration for the original sediments. The fate-controlling effect of contaminants in TTS application for soil amendment should be evaluated combining sorption/desorption and sorption thermodynamic studies.  相似文献   

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