根际土壤磷的动态

养分的有铲性是由土壤物理、化学和生物学特性，特别是根系主导的根际动态所决定的的，根系引起根际ＰＨ值和Ｅｈ、根分泌物以及由此而引起微生物种群、数量和活性的改变，从根本上决定着根际养分的动态而根系的动态又受植物生长的调控。根际微生态系统直接影响到土壤养分向根系的转移和被根系的吸收利用。因此，研究养分在根系－－土壤微环境中的动态是十分重要的。     

根系分泌物主要作用及解析技术进展

根系分泌物是植物保持根际微生态系统活力的关键因素，也是根际物质循环的重要组成部分，对根际土壤生态环境中的物质循环具有重要的驱动作用。根系分泌物可以刺激微生物生长，增强其活性，加速根际养分循环，增加土壤养分利用率，并在小规模空间引起温室气体通量的变化。此外，它也是植物参与竞争的重要策略，植物通过根分泌物以获取种间长期生存的养分，甚至分泌对自身有害的化感物质来排挤其他植物，实现自我生存，即使存在自毒作用或引起连作障碍等。植物的健康生长依赖于自身与土壤微生物复杂动态群落的相互作用，但是根际微生物群落结构和组成却又受植物物种、植物生长期、土壤性质、功能基因等因素影响，这些因素的动态变化可能导致根系分泌物的多样化，从而形成复杂多变的根系分泌物与植物的关系，进而影响植物的健康生长。目前，对植物根系分泌物的研究是土壤生态学、植物营养与代谢等领域的研究热点，且随着分析技术手段的快速发展，根系分泌物相关研究也逐渐深入，进一步揭示植物与微生物间的协同作用机理对农、林等行业生产具有重要的指导意义。     

植物根系分泌物与根际营养关系评述

根系分泌物（ｒｏｏｔ ｅｘｕｄａｔｅｓ,ＲＥ）主要有粘胶、外酶、有机酸、糖、酚及各种氨基酸。不同营养基因型的植物,ＲＥ级分明显不同,存在养分和环境胁迫时,植物通过增加粘胶、酶及某些有机酸的分泌量以适应变化的环境。ＲＥ也是植物改善根际营养环境的重要手段。ＲＥ可改善土壤物理结构,促进矿物风化、提高土壤ＣＥＣ,影响土壤ｐＨ、土壤矿物表面吸附性能及土壤生物学性质。ＲＥ还存化根际土壤养分,促进植物对养分吸收     

施肥对婆婆纳、离子芥、小花糖芥3种麦田杂草根际pH的影响

根际是受根系影响而在物理、化学和生物学性质等方面均不同于土体的极小部分土壤区域.研究表明:植物生长过程中,由于根系的代谢作用而向根外排泄H 或HCO3-,使根际土壤pH发生较大变化.而根际土壤的pH直接影响到土壤养分的活性和生物有效性.故不同植物根际土壤的pH状况可反映出它们对土壤氮、磷、钾养分吸收利用能力的相对大小.     

褪黑素调控根系生长和根际互作的机制研究进展

【目的】根系生长和根际互作是影响植物对土壤养分吸收的关键因子。根系在土壤中穿插生长，不断改变其形态可塑性，进而改变根系构型，扩大与土壤的接触面积以获取所需养分。同时根系的生理可塑性协同根系形态可塑性显著影响根际互作效应，为植物经济高效获取养分资源提供可能。探究褪黑素等内源生长调节因子对根系形态和生理可塑性的调控机制，揭示通过最大化根际效应强化根际互作的有效途径，对集约化作物体系提高养分利用效率，促进绿色增产增效，具有重要的理论与实践意义。主要进展褪黑素作为新型植物生长调节信号分子，在盐害、干旱和低温等非生物胁迫中具有增强植物抗逆性、改善植物生长等重要调节作用。褪黑素显著改变根系生长，对植物主根生长主要表现为抑制作用，对侧根及不定根的发育和生长具有浓度依赖性调节，从而深刻影响植物根系构型。褪黑素调控根系生长的机制尚不清楚，总结已有进展表明:一方面褪黑素调节光周期，影响光合产物的运输和糖信号，从而调控地下部碳分配和根系生长；另一方面，褪黑素还能与生长素等植物激素互作，参与激素对植物生长调控的信号通路，从而对植物的生长发育和新陈代谢产生影响。这些进展对深入揭示褪黑素调控根系生长发育的机制提供了重要依据。问题与展望根系的生长发育以及根系构型的改变显著影响根际过程和根际互作，褪黑素作为调控因子在不同养分环境条件下显著影响根系的形态可塑性。然而，褪黑素在根际过程和根际互作中的作用机制并不清楚，有关研究亟待加强。深入探究褪黑素参与根际互作的机制，理解褪黑素调控根系生长和根际过程的作用途径，可为集约化农业体系下精准调控作物根系生长，强化根际互作，提高养分利用效率提供科学依据。     

外源稀土作用下根–土界面元素转化、分布及其植物有效性的研究进展

外源稀土（RE）可导致根-土界面物理、化学及生物学特性发生根本性变化,特别是根系主导的根际动态过程的变化。如施用不同剂量RE条件下,稀土元素（REE）与根系的相互作用使根系生长、酶活性、细胞质膜透性等受到不同程度的影响。根系生长、酶活性的变化反映了植物可能通过根系形态学、生理学的适应性和非适应性变化机制来改变根系吸收养分、REE及重金属离子的能力,直接影响根际离子进入根系中的含量;而根系细胞质膜透性的变化则反映了植物可能通过根系分泌作用的适应性和非适应性变化机制来改变根系有机酸、质子等的分泌状况,使之作用于根际环境,制约养分、REE及重金属元素在根际的形态转化与迁移分布模式,从而间接影响根际离子进入根系中的含量。本文从外源RE对根系生长状况和酶活性的影响;对根系细胞质膜透性和分泌作用的影响;对根际养分、REE及重金属元素动态的影响;对根系养分、REE及重金属元素吸收分布的影响等4个方面的国内外文献出发,就土壤-植物系统中外源RE作用下根-土界面养分、REE及重金属元素的转化、分布及其植物有效性的响应变化与相关机制做出综述,同时提出目前研究中存在的问题,对今后的研究方向进行展望。     

集约化互作体系植物根系高效获取土壤养分的策略与机制

【目的】植物根系的形态与生理变化是植物从土壤中高效获取养分资源的重要机制，由相同物种或不同物种组成的互作体系中植物根系对养分的吸收利用受相邻植物竞争的强烈影响，阐明互作体系不同竞争条件下植物根系获取养分的策略并揭示其作用机制，这是基于根系觅食行为探讨养分高效利用的根际调控途径与技术措施的重要理论基础。主要进展根系属性的互补性有利于降低根系间对养分的竞争。根系构型的互补性，例如深根系与浅根系植物互作，促进个体植株对土壤剖面不同深度养分的吸收利用；由根系可塑性介导的水平方向上根系空间分布的互补性，提高了植物根系对同一土层不同空间位点土壤养分的挖掘；个体植株根系形态属性与相邻植物根际生理过程的互补性促进根系对不同形态养分的利用。互作体系根系获取养分的策略具有高度互补性，这有助于提高整个作物系统的养分利用效率，进而提高生产力。根系空间生态位的分离 (包括垂直与水平方向) 以及根际生物化学特征生态位的分离，是驱动互作体系根系高效获取养分资源的主要机制。合理的根层调控可以提高植物根系挖掘土壤养分的能力；优化互作体系物种的搭配能充分发挥根的互作效能，提高养分利用的生物潜力。问题与展望今后应进一步针对集约化高投入作物体系，通过管理根层养分供应和物种间的互作效应，强化根际养分信号的调控作用，调节根系形态与生理特性，降低种间竞争，增强种间互利，以最大化根系和根际的生物学潜力，提高养分利用效率和作物产量，为实现以节肥增效为核心的可持续集约化作物生产提供重要的调控策略与途径。     

植物根际微生物调控根系构型研究

植物根系构型即根系在其生长介质中的生长与分布,包括根系长度、根系分支和根系生物量等,能够将植物固定在土壤中并有效吸收水分和矿质养分,直接影响植物的生长和发育。根系构型受多种因素的影响,包括土壤水分、养分和根际微生物,传统方式主要依靠化学肥料增加土壤养分进而改善根系生长,但是化学肥料会对环境造成危害,根际微生物作为植物的“第二基因组”,能够改善初生根、侧根和根毛的发育,促进植物的生长和根际养分吸收,近年来基因组学−代谢组学、基因组学−转录组学等多组学关联技术的应用揭示了微生物的促生机制,为微生物菌剂的开发提供了新思路。基于该领域的研究现状,本文阐述了根际微生物（AMF、PGPR、根瘤菌）对根构型的调控机制包括激素调控、固氮、溶磷、释放挥发性有机化合物四个方面,并描述它们通过这四种机制增加植物根系长度、根系分支,促进根毛发育的调控效应,基于上述结论,植物根际微生物可以有效改善根系生长,但实际应用效果还有待研究,量化不同机制的相对贡献率以及提高微生物菌剂在实际应用中的稳定性是后续研究的重点。     

水稻根系对氮素损失的影响

植物根系的呼吸、水分和养分的吸收、根系分泌物以及死亡根皮和根毛的脱落等,常引起土壤性状的变化,从而形成了根际土壤特殊的微生物活动环境。     

植物的磷素营养和土壤磷的生物有效性

本文介绍了近年来植物磷素营养研究的发展趋势,强调了开展不同基因型作物品种耐低磷机理研究的重要性;阐述了磷有效性品种生产率和根形态的差异、吸收动力学参数与耐低磷的关系、缺磷的酶促适应性,以及作物根系分泌物的作用等。对土壤根际磷有效的影响因素(如根际pH、磷亏缺梯度、有效扩散系数、缓冲力等)进行了综合讨论。     

Physical,Chemical, and Biological Changes in the Rhizosphere and Nutrient Availability

The rhizosphere is the soil zone adjacent to plant roots which is physically, chemically, and biologically different from bulk or non-rhizosphere soil. Adaptative mechanisms of plants influence physical (temperature, water availability, and structure), chemical [pH, redox potential, nutrient concentration, root exudates, aluminum (Al) detoxification and allelopathy], and biological properties (microbial association) in the rhizosphere. These changes affect nutrient solubility, transport, and uptake and ultimately plant growth. Major rhizosphere changes are synthesized and their influence on nutrient availability is discussed. In the last decade, significant progress has been made in understanding the rhizosphere environment and nutrient availability. However, the subject matter is very complex and more research is needed to understand the interaction between the plant, the rhizosphere environment, and nutrient availability.     

Rhizosphere interactions between microorganisms and plants govern iron and phosphorus acquisition along the root axis - model and research methods

Iron and phosphorus availability is low in many soils; hence, microorganisms and plants have evolved mechanisms to acquire these nutrients by altering the chemical conditions that affect their solubility. In plants, this includes exudation of organic acid anions and acidification of the rhizosphere by release of protons in response to iron and phosphorus deficiency. Grasses (family Poaceae) and microorganisms further respond to Fe deficiency by production and release of specific chelators (phytosiderophores and siderophores, respectively) that complex Fe to enhance its diffusion to the cell surface. In the rhizosphere, the mutual demand for Fe and P results in competition between plants and microorganisms with the latter being more competitive due to their ability to decompose plant-derived chelators and their proximity to the root surface; however microbial competitiveness is strongly affected by carbon availability. On the other hand, plants are able to avoid direct competition with microorganisms due to the spatial and temporal variability in the amount and composition of exudates they release into the rhizosphere. In this review, we present a model of the interactions that occur between microorganisms and roots along the root axis, and discuss advantages and limitations of methods that can be used to study these interactions at nanometre to centimetre scales. Our analysis suggests mechanisms such as increasing turnover of microbial biomass or enhanced nutrient uptake capacity of mature root zones that may enhance plant competitiveness could be used to develop plant genotypes with enhanced efficiency in nutrient acquisition. Our model of interactions between plants and microorganisms in the rhizosphere will be useful for understanding the biogeochemistry of P and Fe and for enhancing the effectiveness of fertilization.     

Rhizospheric organic compounds in the soil–microorganism–plant system: their role in iron availability

Poor iron (Fe) availability in soil represents one of the most important limiting factors of agricultural production and is closely linked to physical, chemical and biological processes within the rhizosphere as a result of soil–microorganism–plant interactions. Iron shortage induces several mechanisms in soil organisms, resulting in an enhanced release of inorganic (such as protons) and organic (organic acids, carbohydrates, amino acids, phytosiderophores, siderophores, phenolics and enzymes) compounds to increase the solubility of poorly available Fe pools. However, rhizospheric organic compounds (ROCs) have short half‐lives because of the large microbial activity at the soil–root interface, which might limit their effects on Fe mobility and acquisition. In addition, ROCs also have a selective effect on the microbial community present in the rhizosphere. This review aims therefore to unravel these complex dynamics with the objective of providing an overview of the rhizosphere processes involved in Fe acquisition by soil organisms (plants and microorganisms). In particular, the review provides information on (i) Fe availability in soils, including mineral weathering and Fe mobilization from soil minerals, ligand and element competition and plant‐microbe competition; (ii) microbe–plant interactions, focusing on beneficial microbial communities and their association with plants, which in turn influences plant mineral nutrition; (iii) plant–soil interactions involving the metabolic changes triggered by Fe deficiency and the processes involved in exudate release from roots; and (iv) the influence of agrochemicals commonly used in agricultural production systems on rhizosphere processes related to Fe availability and acquisition by crops.     

豆科禾本科作物间作的根际生物过程研究进展

间作作为一种可持续发展的种植模式不仅具有产量和养分获取的优势,而且能够保证粮食安全、降低作物减产风险。在众多间作组合中,豆科禾本科作物间作由于种间促进及生态位互补作用,而在世界范围内被广泛应用。根际是作物-土壤-微生物相互作用的界面,是养分、水分及有害物质从土壤进入作物系统参与食物链物质循环的必经门户,在根际中所发生的生物过程不仅决定着养分的供应量和有效性,而且也影响着作物的生产力和养分利用效率。因此,本文从豆科禾本科间作的根际生物过程角度出发,综述了豆科禾本科间作对根系形态、根际微生物、根系分泌物及其生态效应的研究进展,为豆科禾本科间作体系在修复重金属污染土壤、提高土壤中养分有效性以及植物遗传改良等方面的应用提供理论依据。     

Intercropping promotes the ability of durum wheat and chickpea to increase rhizosphere phosphorus availability in a low P soil

Cereal–legume intercropping can promote plant growth (i.e. facilitation) through an increase in the amount of phosphorus (P) taken up, especially in low P soils. The aim of this study was to test the hypothesis that these positive interactions are supported by rhizosphere processes that increase P availability, such as root-induced pH changes. In neutral and alkaline soils legumes are assumed to increase inorganic P availability by rhizosphere acidification due to N₂ fixation which benefit to the intercropped cereal. Growth, P uptake, changes in inorganic P availability and pH in the rhizosphere of intercropped species were thus investigated in a greenhouse pot experiment with durum wheat and chickpea either grown alone or intercropped. We used a neutral soil from a P fertilizer long-term field trial exhibiting either low (−P) or high (+P) P availability. Phosphorus availability was increased in the rhizosphere of both species, especially when intercropped in −P. Such increase was associated with alkalization. Rhizosphere pH changes could not fully explain the observed changes of P availability though. Low rates of N₂ fixation may explain why no rhizosphere acidification was observed. Increases in P availability did not lead to enhanced P uptake but growth promotion was observed for durum wheat intercropped with chickpea in −P soil. Our hypothesis of an increase in inorganic P availability in intercropping as a consequence of root-induced acidification by the legume was not validated, and we suggested that root-induced alkalization was involved instead, as well as other root-induced processes. Thus, the cereal through rhizosphere alkalization may also enhance P uptake and growth of the intercropped legume. Facilitation can thus occur in both ways.     

玉米根鞘改变土壤粒径及养分有效性

Root exudates,microorganism colonization and soil aggregates together form the rhizosheath,a special cylinder of micro-ecosystem adhering to the root surface.To study how the rhizosheath affects soil structure and nutrient distribution,we analyzed the impact of maize rhizosheath on soil particle size and nutrient availability in pot and field experiments.The results showed that there was a significant size decrease of soil particles in the rhizosheath.Meanwhile,the soil mineral nitrogen in the rhizosheath was significantly higher than that in the rhizosphere or bulk soil at tasseling and maturity stages of maize.The contents of Fe and Mn were also differentially altered in the rhizosheath.Rhizosheath development,indicated by a dry weight ratio of rhizosheath soil to the root,was relatively independent of root development during the whole experimental period.The formation of maize rhizosheath contributed to the modulation of soil particle size and nutrient availability.The subtle local changes of soil physical and chemical properties may have profound influence on soil formation,rhizospheric ecosystem initiation,and mineral nutrient mobilization over the long history of plant evolution and domestication.     

Rhizosphere effect of three plant species of environment under periglacial conditions (Majella Massif,central Italy)

The chemical, physical and biological processes occurring in the rhizosphere can influence plant growth by modifying root associated microorganisms and nutrient cycles. Although rhizosphere has been widely investigated, little is known about the rhizosphere effect of pioneer plants in soils of periglacial environments. The knowledge of the processes controlling soil–plant relationships in these severe environments may help understanding the ecological evolution of newly deglaciated surfaces. We selected three plants [Helianthemum nummularium (L.) Mill. subsp. grandiflorum (Scop.), Dryas octopetala (L.), and Silene acaulis (L.) Jacq. subsp. cenisia (Vierh.) P. Fourn.] that sparsely occupy deglaciated areas of central Apennines (Italy), with the aim to assess changes between rhizosphere and bulk soil in terms of physical, chemical, and biological properties. The three plants considered showed to have different rhizosphere effect. Helianthemum induced a strong rhizosphere effect through a synergistic effect between root activity and a well adapted rhizosphere microbial community. Dryas did not foster a microbial community structure specifically designed for its rhizosphere, but consumes most of the energetic resources supplied by the plant to make nutrients available. Conversely to the other two species, Silene produced slight soil changes in the rhizosphere, where the microbial community had a structure, abundance and activity similar to those of the bulk soil. The ability to colonize harsh environments of Silene is probably linked to the shape and functions of its canopy rather than to a functional rhizosphere effect.This study showed that the rhizosphere effect differed by species also under high environmental pressure (periglacial conditions, poorly developed soil), and the activity of roots and associated microbial community is decisive in modifying the soil properties, so to create a suitable environment where plants are able to grow.