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1.
郭庆荣  张秉刚 《生态科学》1996,15(2):112-116
土壤植物系统是土壤—植物—大气连续体中的一个重要的子系统,该系统中的植物根系吸收土壤水份的研究已受到国内外的普遍重视,成为旱地农业生态系统中最为活跃的研究课题之一。从土壤—植物—大气连续体入手,对植物根系吸收土壤水份的影响因素,植物根系吸收土壤水份的微观模型及宏观模型等,进行了介绍和评述  相似文献   

2.
臭氧浓度升高对盆栽小麦根系和土壤微生物功能的影响   总被引:11,自引:0,他引:11  
模拟研究了臭氧浓度升高(日变化熏蒸方式)对小麦根系和土壤微生物活性的影响。实验分3个处理,即空气对照(CF,臭氧浓度约4~10nl·L^-1),臭氧浓度Ⅰ(OⅠ,8h平均75nl·L^-1),臭氧浓度Ⅱ(OⅡ,8h平均110nl·L^-1)。结果表明,臭氧浓度升高后小麦茎叶、根系生物量以及根冠比都会降低,根系活力更是显著低于空气对照,可见臭氧对植物地下部分的影响是显著的。与对照相比,低浓度O3(75nl·L^-1)对根际土和非根际土的微生物生物量碳没有什么影响;而较高的O3浓度(110nl·L^-1)会造成根际土微生物生物量碳降低9.3%,非根际土微生物生物量碳降低5.3%,说明高浓度臭氧抑制土壤微生物的量。臭氧浓度升高后小麦根际土壤微生物利用单一碳源的能力(AWCD)都明显低于对照;低浓度的臭氧对土壤微生物的多样性指数和丰富度指数都没有显著影响,而浓度较高的臭氧则显著降低了根际土微生物的多样性指数,而对丰富度指数没有显著影响,且也没有发现O3浓度升高对非根际土微生物的影响。可见,臭氧主要影响根际土壤微生物而对非根际土壤微生物影响不大,且只有在高浓度的臭氧处理下才会显著降低根际土壤微生物的多样性指数。  相似文献   

3.
大气CO2浓度升高对植物根系的影响   总被引:3,自引:0,他引:3  
植物长期生长在CO2浓度不断升高的环境中,其结构和功能都将受到影响,这种影响不仅表现在植物的地上部分,同时也表现在植物的地下部分(根系),尤其是细根的长度、直径、产量、周转以及根与枝的分配模式等方面。植物根系结构和功能的改变影响植物地上部分和生态系统物质循环中的碳动态及土壤中碳库的变化。目前有关大气CO2浓度升高对根系动态影响的研究报道主要包括大气CO2浓度升高对根系结构(直径、分枝、长度、数量等)和根系生理(周转率、产量、碳分配模式等)的影响2个方面。目前,该领域研究还存在一些不足,例如在CO2浓度升高条件下,对植物根系内部的调控机制,以及由其引起的物质循环和能量流动的动态变化的了解较少;至今没有令人信服的证据说明大气CO2浓度升高使根系周转升高还是降低。今后应加强研究在CO2浓度升高条件下根系的周转变化和光合产物分配模式变化,CO2浓度升高和外界环境因素的共同作用对根系的影响,以及采用不同研究方法和研究对象在不同立地条件下开展升高CO2浓度对根系影响的对比研究等。  相似文献   

4.
植物根系分泌物对土壤污染修复的作用及影响机理   总被引:4,自引:0,他引:4  
王亚  冯发运  葛静  李勇  余向阳 《生态学报》2022,42(3):829-842
生物修复是一种经济环保的土壤修复技术。根系分泌物是利用生物修复污染土壤过程中的关键物质,也是植物与土壤微生物进行物质交换和信息传递的重要载体,在植物响应污染物胁迫中扮演重要角色。研究植物根系分泌物对土壤污染修复的作用和影响机理,是深入理解植物和微生物环境适应机制的重要途径,对促进生物修复污染土壤有重要指导意义。从污染物胁迫对根系分泌物的影响、根系分泌物对土壤污染物环境行为的影响、根系分泌物在调控污染土壤中根际微生物群落结构和多样性中发挥的作用等几个方面综述了根系分泌物对土壤污染修复的影响及内在机制。研究结果表明,根系分泌物在降低重金属对植物的毒性、加速有机污染物降解等方面有非常重要的作用。根系分泌物对土壤微生物的丰度和多样性均有显著影响,其与根际微生物互作在土壤污染物的消减中发挥了重要的调控作用。在此基础上,提出了以往研究中的不足,并对污染物胁迫下根系分泌物未来研究的方向和趋势进行了展望。  相似文献   

5.
我国土壤重金属污染问题日益突出。作为一种绿色、安全的生物修复技术,植物修复技术备受关注。根系分泌物作为植物-土壤-微生物三者物质交换与信息传递的重要载体,是植物响应外界胁迫的重要生理生态指征,在植物修复过程中发挥关键作用。研究表明,根系分泌物能够有效调控根际微环境,提升植物抗逆能力,影响重金属在根际微域中的环境行为。传统的根际生态研究更多聚焦在养分调控等方面,而关于根系分泌物在污染场地生态修复中的作用机制研究相对较少。本文综述了根系分泌物对土壤理化性质、土壤微生物、植物生理代谢过程以及重金属在土壤-植物系统中迁移转化等方面的影响,系统总结了植物根系分泌物响应重金属胁迫的生理生态机制,并对未来土壤重金属污染生态修复研究方向进行了展望。  相似文献   

6.
土壤养分空间异质性与植物根系的觅食反应   总被引:41,自引:5,他引:41  
植物在长期进化过程中,为了最大限度地获取土壤资源,对养分的空间异质性产生各种可塑性反应.包括形态可塑性、生理可塑性、菌根可塑性等.许多植物种的根系在养分丰富的斑块中大量增生,增生程度种间差异较大,并受斑块属性(斑块大小、养分浓度)、营养元素种类和养分总体供应状况的影响.植物还通过调整富养斑块中细根的直径、分枝角、节问距以及空间构型来实现斑块养分的高效利用.根系的生理可塑性及菌根可塑性可能在一定程度上影响其形态可塑性.生理可塑性表现为处于不同养分斑块上的根系迅速调整其养分吸收速率,从而增加单位根系的养分吸收,对在时间上和空间上变化频繁的空间异质性土壤养分的利用具有重要意义,可在一定程度上弥补根系增生反应的不足.菌根可塑性目前研究较少,一些植物种的菌根代替细根实现在富养斑块中的增生.菌根增生的碳投入养分吸收效率较高、根系增生对增加养分吸收的作用较复杂,取决于养分离子在土壤中的移动性能以及是否存在竞争植物;对植物生长(竞争能力)的作用因种而异,一些敏感种由此获得生长效益,而其它一些植物种受影响较小.植物个体对土壤养分空间异质性反应能力和生长差异,影响其在群落中的地位和命运,最终影响群落组成及其结构.  相似文献   

7.
植物根系分泌物主要生态功能研究进展   总被引:1,自引:0,他引:1  
根系分泌物在植物根系-土壤-微生物互作过程及其生态反馈机制中发挥重要作用。在植物根际复杂网络互作过程中, 根系分泌物被认为是“根际对话”的媒介, 其在调控植物适应微生境、缓解根际养分竞争及构建根际微生物群落结构方面意义重大。该文结合国内外该领域主要研究成果, 综述了根系分泌物对植物生长、土壤微生物特性及土壤养分循环的影响, 并展望了未来根系分泌物的研究方向。  相似文献   

8.
碳输入方式对森林土壤碳库和碳循环的影响研究进展   总被引:8,自引:2,他引:6  
Wang QK 《应用生态学报》2011,22(4):1075-1081
凋落物和植物根系是森林土壤有机碳的主要来源.综述了不同碳输入方式对土壤全碳、微生物生物量碳和可溶性有机碳等碳库组分及土壤呼吸影响的研究进展.不同地区、不同森林土壤有机碳对碳输入的响应程度不同,且采用添加和去除凋落物,以及去除根系方法(DIRT)对土壤碳的影响具有树种差异和区域差异.目前主要侧重于土壤呼吸和碳库组分的研究,亟需开展对土壤碳的结构类型和稳定性,以及土壤生物尤其是土壤动物的响应机制的相关研究.  相似文献   

9.
宁南山区典型植物根系分解特征及其对土壤养分的影响   总被引:1,自引:0,他引:1  
杨轩  李娅芸  安韶山  曾全超 《生态学报》2019,39(8):2741-2751
根系分解是陆地生态系统碳和养分循环的重要地下生态过程,研究宁南山区典型植物根系分解特征及其对土壤养分的影响,能够丰富和完善陆地生态系统的物质和能量循环机制,为我国黄土高原植被恢复过程中植物与土壤之间的养分循环提供依据。连续2年研究了宁南山区3种典型植物(长芒草、铁杆蒿和百里香)根系的分解特征及其对土壤养分的影响。结果表明,长芒草、铁杆蒿和百里香根系年分解指数(K)分别0.00891、0.01128、0.01408,分解速率依次表现为百里香铁杆蒿长芒草。分解16个月后3种典型植物根系释放大量养分,其中碳的释放量在57.05—124.39 g/kg;氮的释放量在0.12—0.47 g/kg。3种典型植物根系对土壤养分的影响主要表现为:试验结束时,0—5 cm表层土壤有机碳含量提高了0.17—0.35 g/kg,5—20 cm土层土壤有机碳含量提高了0.26—0.35 g/kg。相关性分析可知,植物根系养分释放量与土壤养分含量之间存在一定的负相关关系,当土壤养分含量较低时,根系会增加养分释放量进行补充。由此可知,根系分解提高了土壤养分含量,有效的促进了养分在根系-土壤中的循环。  相似文献   

10.
根系间的相互作用——竞争与互利   总被引:23,自引:4,他引:19  
陈伟  薛立 《生态学报》2004,24(6):1243-1251
植物根系间的相互作用分为竞争和互利两种形式 ,它是决定植物群落动态变化和群落结构的重要因素。根系间的竞争包括植株个体自身根系的竞争以及个体与个体根系间 (同种或异种 )的竞争两方面 ,前者的发生在农林系统中是不可避免的并且很难调控 ,后者可以分为种间植物根系的竞争和种内植物根系的竞争。还阐述了根系的竞争能力和与其密切相关的根系生长率、根组织的新陈代谢、植物的生长形式和根系的空间结构等植物特性 ,同时介绍了根系对水和养分的竞争机理、形式、影响以及竞争强度计算方法。接着具体分析包括根系错位在内的各种根系互利现象和相关机理。影响根系间相互作用的限制性因子有土壤营养的异质性、大气 CO2 浓度、地下草食生物、根系生产力和生物量、根系结构、形态和生理调节、土壤养分的扩散性以及植物间距等。随着科技的进步和各门学科的发展 ,未来根系的研究方向主要体现在结合实践优化农林系统中不同物种间的作用关系、预测根系竞争在全球气候变化下的发展规律、更新实验研究方法及手段研究作用机理等 3个方面。  相似文献   

11.
The morphology of roots and root systems influences the efficiency by which plants acquire nutrients and water, anchor themselves and provide stability to the surrounding soil. Plant genotype and the biotic and abiotic environment significantly influence root morphology, growth and ultimately crop yield. The challenge for researchers interested in phenotyping root systems is, therefore, not just to measure roots and link their phenotype to the plant genotype, but also to understand how the growth of roots is influenced by their environment. This review discusses progress in quantifying root system parameters (e.g. in terms of size, shape and dynamics) using imaging and image analysis technologies and also discusses their potential for providing a better understanding of root:soil interactions. Significant progress has been made in image acquisition techniques, however trade‐offs exist between sample throughput, sample size, image resolution and information gained. All of these factors impact on downstream image analysis processes. While there have been significant advances in computation power, limitations still exist in statistical processes involved in image analysis. Utilizing and combining different imaging systems, integrating measurements and image analysis where possible, and amalgamating data will allow researchers to gain a better understanding of root:soil interactions.  相似文献   

12.
The aim was to analyze functional changes in the mycorrhizosphere (MR) of juvenile spruce and beech grown in a mixture under ambient and twice ambient ozone and inoculated with the root pathogen Phytophthora citricola. The phytotron experiment was performed over two vegetation periods, adding the pathogen at the end of the first growing season. Root biomass data suggest that the combined treatment affected spruce more than beech and that the negative influence of ozone on stress tolerance against the root pathogen P. citricola was greater for spruce than for beech. In contrast, beech was more affected when the pathogen was the sole stressor. The functional soil parameter chosen for studies of MR soil samples was activity of extracellular enzymes. After the first year of ozone exposure, MR soil samples of both species showed increased activity of almost all measured enzymes (acid phosphatase, chitinase, beta-glucosidase, cellobiohydrolase) in the O3 treatment. Species-specific differences were observed, with a stronger effect of P. citricola on beech MR and a stronger ozone effect on spruce MR. In the second year, the effects of the combined treatment (ozone and P. citricola) were a significant increase in the activity of most enzymes (except cellobiohydrolase) for both tree species. The results indicated that responsiveness of MR soils towards ozone and P. citricola was related to the severity of infection of the plants and the reduction of belowground biomass, suggesting a strong, direct influence of plant stress on MR soil enzyme activity. Additional research is needed using different species and combined stresses to determine the broader ecological relevance of shifts in rhizosphere enzymes.  相似文献   

13.
近地层臭氧(O3)浓度升高作为全球气候变化的重要因素之一,对土壤生态环境和农作物生长发育造成了很大影响.本研究采用开顶式气室(OTCs)法,探究臭氧浓度升高对小麦不同生育期(分蘖期、拔节期、孕穗期和成熟期)根际土壤酶活性(过氧化氢酶、多酚氧化酶、脱氢酶和转化酶)和有机酸含量(草酸、柠檬酸和苹果酸)的影响规律,并结合根际土壤理化性质、植株根系生长状况等分析其产生影响的原因.结果表明: O3浓度升高不同程度地提高了小麦成熟期土壤过氧化氢酶、多酚氧化酶、脱氢酶和转化酶活性,其中过氧化氢酶和多酚氧化酶活性提高达显著水平;在抽穗期,脱氢酶和转化酶活性因臭氧浓度升高而显著提高,增幅最高可达76.7%.在成熟期,O3浓度升高显著提高了根际土壤中柠檬酸和苹果酸含量;显著降低了根际土壤pH、电导率、总碳和总氮含量,增加了土壤氧化还原电位(Eh);显著降低了小麦根系生物量、总根长和根总表面积,而增加了根平均直径.  相似文献   

14.
Lamont  Byron B. 《Plant and Soil》2003,248(1-2):1-19
Hairy rootlets, aggregated in longitudinal rows to form distinct clusters, are a major part of the root system in some species. These root clusters are almost universal (1600 species) in the family Proteaceae (proteoid roots), with fewer species in another seven families. There may be 10–1000 rootlets per cm length of parent root in 2–7 rows. Proteoid roots may increase the surface area by over 140× and soil volume explored by 300× that per length of an equivalent non-proteoid root. This greatly enhances exudation of carboxylates, phenolics and water, solubilisation of mineral and organic nutrients and uptake of inorganic nutrients, amino acids and water per unit root mass. Root cluster production peaks at soil nutrient levels (P, N, Fe) suboptimal for growth of the rest of the root system, and may cease when shoot mass peaks. As with other root types, root cluster production is controlled by the interplay between external and internal nutrient levels, and mediated by auxin and other hormones to which the process is particularly sensitive. Proteoid roots are concentrated in the humus-rich surface soil horizons, by 800× in Banksia scrub-heath. Compared with an equal mass of the B horizon, the A1 horizon has much higher levels of N, P, K and Ca in soils where species with proteoid root clusters are prominent, and the concentration of root clusters in that region ensures that uptake is optimal where supply is maximal. Both proteoid and non-proteoid root growth are promoted wherever the humus-rich layer is located in the soil profile, with 4× more proteoid roots per root length in Hakea laurina. Proteoid root production near the soil surface is favoured among hakeas, even in uniform soil, but to a lesser extent, while addition of dilute N or P solutions in split-root system studies promotes non-proteoid, but inhibits proteoid, root production. Local or seasonal applications of water to hakeas initiate non-proteoid, then proteoid, root production, while waterlogging inhibits non-proteoid, but promotes proteoid, root production near the soil surface. A chemical stimulus, probably of bacterial origin, may be associated with root cluster initiation, but most experiments have alternative interpretations. It is possible that the bacterial component of soil pockets rich in organic matter, rather than their nutrient component, could be responsible for the proliferation of proteoid roots there, but much more research on root cluster microbiology is needed.  相似文献   

15.
Soil compaction is a widespread cause of reduced plant productivity. If the effects of soil compaction on plant growth are to be reproduced in simulation models, then the processes through which compaction reduces root elongation must be expressed mathematically and then tested against experimental data. The mathematical theory by which these processes may be represented is given in the accompanying article. In this article, the behavior of a simulation model based on this theory is tested against data for root growth and soil gas concentration recorded from soil columns of which the middle layers were compacted to different bulk densities. The model was able to reproduce the failure of the root system to penetrate the compacted middle layer within the period of the experiment when bulk density exceeded 1.55 Mg m-3. The model also reproduced decreases in O2 concentrations, and increases in CO2 concentrations, in the atmospheres of the compacted layer and of the uncompacted layer below it as bulk density of the compacted layer increased. The simulated time course of O2 and nutrient uptake and of O2 concentrations in the compacted layer at different depths is presented and its consistency with experimental findings is examined. As part of a larger ecosystem model, this model will be useful in estimating site-specific effects of soil compaction on carbon cycling in agroecosystems.  相似文献   

16.
土壤有效氮及其相关因素对植物细根的影响   总被引:7,自引:0,他引:7  
细根(直径≤2mm)作为植物吸收水分和养分的主要器官之一,在陆地生态系统养分循环和能量流动中起重要作用。开展土壤有效氮变化对植物细根影响研究对于了解全球气候变化条件下的陆地生态系统养分循环具有重要意义。本文就相关研究进行了综述:1)土壤有效氮变化对植物细根生长、发育、寿命及呼吸的直接影响;2)土壤质地、温度、大气CO2浓度和氮沉积等相关因素对植物细根的影响。由于研究方法及物种间差异等的影响,研究结果不尽相同。今后,应在不同空间尺度上深入研究土壤有效氮对植物细根的影响,而植物细根-土壤-微生物三者间相互关系变化对土壤氮变化的潜在响应将可能成为今后研究的热点问题之一。  相似文献   

17.
草地早熟禾草坪土壤水分动态与根系生长分布   总被引:13,自引:0,他引:13  
孙强  韩建国  刘帅  周莉华 《生态学报》2005,25(6):1306-1311
对草地早熟禾草坪土壤水分动态和根系生长发育状况进行研究,结果发现不同土壤层次水分变化有所不同,0~15cm变化最大,15~30cm次之,30cm以下土层水分变化不大;草地早熟禾的根系生长呈现双峰曲线模式,5月中旬和8月中下旬总根量处于峰值;其主体根系主要分布在0~30cm土层内,占总根量的85%以上;根重密度随土层深度呈指数衰减关系,0~30cm土层下降幅度较大,30cm以下土层根重密度相差不大;在0~30cm土层内不同层次根量占总根量的比例在不同时期亦有差异,春秋季节10~20cm和20~30cm土层内根量比例较大,说明此时期主体根系分布在较深的土层;综合分析认为草地早熟禾草坪主要利用土壤浅层水分,在降雨较少的春秋季节,根系较深,适宜深层灌溉,在降雨频繁的夏季,根系较浅,适宜浅层灌溉。  相似文献   

18.
We present a simple framework for modelling root growth and distribution with depth under varying soil water conditions. The framework considers the lateral growth of roots (proliferation) and the vertical extension of roots (root front velocity). The root front velocity is assumed to be constant when the roots descend into an initially wet soil profile. The lateral growth of roots is governed by two factors: (1) the current root mass or root length density at a given depth, and (2) soil water availability at that depth.Under non-limiting soil water conditions, the increase in root mass at any depth is governed by a logistic equation so that the root length density (R v) cannot exceed the maximum value. The maximumR v, is assumed to be the same for all depths. Additional dry matter partitioned to roots is initially distributed according to the current root mass at each depth. As the root mass approaches the maximum value, less dry matter is partitioned to that depth.When soil water is limiting, a water deficit factor is introduced to further modify the distribution of root dry matter. It is assumed that the plant is an energy minimiser so that more root mass is partitioned to the wetter regions of the soil where least energy will be expended for root growth. Hence, the model allows for enhanced root growth in areas where soil water is more easily available.Simulation results show that a variety of root distribution patterns can be reproduced due to varying soil water conditions. It has been demonstrated that broad patterns of root distribution reported in the literature can also be simulated by the model.  相似文献   

19.
Fine root tumover is a major pathway for carbon and nutrient cycling in terrestrial ecosystems and is most likely sensitive to many global change factors.Despite the importance of fine root turnover in plant C allocation and nutrient cycling dynamics and the tremendous research efforts in the past,our understanding of it remains limited.This is because the dynamics processes associated with soil resources availability are still poorly understood.Soil moisture,temperature,and available nitrogen are the most important soil characteristics that impact fine root growth and mortality at both the individual root branch and at the ecosystem level.In temperate forest ecosystems,seasonal changes of soil resource availability will alter the pattern of carbon allocation to belowground.Therefore,fine root biomass,root length density(RLD)and specific root length(SRL)vary during the growing season.Studying seasonal changes of fine root biomass,RLD,and SRL associated with soil resource availability will help us understand the mechanistic controls of carbon to fine root longevity and turnover.The objective of this study was to understand whether seasonal variations of fine root biomass,RLD and SRL were associated with soil resource availability,such as moisture,temperature,and nitrogen,and to understand how these soil components impact fine root dynamics in Larix gmelinii plantation.We used a soil coring method to obtain fine root samples(≤2 mm in diameter)every month from Mav to October in 2002 from a 17-year-old L.gmelinii plantation in Maoershan Experiment Station,Northeast Forestry University,China.Seventy-two soil cores(inside diameter 60 mm;depth intervals:0-10 cm,10-20 cm,20-30 cm)were sampled randomly from three replicates 25 m×30 m plots to estimate fine root biomass(live and dead),and calculate RLD and SRL.Soil moisture,temperature,and nitrogen(ammonia and nitrates)at three depth intervals were also analyzed in these plots.Results showed that the average standing fine root biomass(live (32.2 g.m-2.a-1)in the middle(10-20 cm)and deep layer (20-30cm),respectively.Live and dead fine root biomass was the highest from May to July and in September,but lower in August and October.The live fine root biomass decreased and dead biomass increased during the growing soil layer.RLD and SRL in May were the highestthe other months,and RLD was the lowest in Septemberdynamics of fine root biomass,RLD,and SRL showed a close relationship with changes in soil moisture,temperature,and nitrogen availability.To a lesser extent,the temperature could be determined by regression analysis.Fine roots in the upper soil layer have a function of absorbing moisture and nutrients,while the main function of deeper soil may be moisture uptake rather than nutrient acquisition.Therefore,carbon allocation to roots in the upper soil layer and deeper soil layer was different.Multiple regression analysis showed that variation in soil resource availability could explain 71-73% of the seasonal variation of RLD and SRL and 58% of the variation in fine root biomass.These results suggested a greater metabolic activity of fine roots living in soil with higher resource availability,which resulted in an increased allocation of carbohydrate to these roots,but a lower allocation of carbohydrate to those in soil with lower resource availability.  相似文献   

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