喀斯特坡地拉巴豆地埂篱根及根-土复合体力学特性

为探索地埂篱在喀斯特坡地水土保持中的价值,在重庆市酉阳县喀斯特顺层坡种植拉巴豆地埂篱,通过对根系灰度扫描、化学成分(木质素、纤维素、半纤维素)测定,单根抗拉试验和根-土复合体抗剪/冲试验,分析拉巴豆地埂篱根及根-土复合体的力学特性及影响因素。结果表明:(1)拉巴豆根系全根指标根长、根表面积、根体积、根重均表现为中坡下坡上坡,优势径级为0.0d≤1.0 mm径级。全根根系纤维素的平均含量较木质素、半纤维素高,且与根系直径呈显著负相关。(2)根系平均极限抗拉力6.77 N、平均抗拉强度29.57 MPa。极限抗拉力与木质素含量呈对数函数正相关、与木质素/纤维素(木纤比)呈线性正相关,抗拉强度与纤维素含量、木纤比分别为对数函数正相关和负相关。(3)上坡位抗剪土样的根体积密度、根重密度和木纤比显著大于中、下坡;而抗冲土样的根体积密度、根重密度、纤维素和半纤维素含量则中坡较优,但不显著。(4)根系能有效提高土体抗剪性能,根-土复合体的内摩擦角与粘聚力均较对照裸地高,但仅上坡粘聚力存在显著性差异(较对照增大45.67%)。内摩擦角和抗冲指数均中坡、下坡较优,粘聚力最优值位于上坡位。根-土复合体的力学特性主要受根体积、根重、根表面积密度和纤维素的影响。综上,拉巴豆根及根-土复合体的力学特性主要贡献径级为0.0d≤1.0 mm径级,中、下坡细根量大且根-土复合体抗冲性能表现较优,上坡根-土复合体抗剪切能力最强,但抗冲性能较弱。在推广拉巴豆地埂篱时,尽量种植于地势较低缓的中、下坡,更能凸显水土保持效益。     

喀斯特坡地2种地埂篱根-土复合体抗剪和抗冲性能综合评价

分析喀斯特地区不同地埂篱根系的形态和力学特性，量化其根-土复合体抗剪和抗冲性能的强弱，探寻该地区地埂篱根系固土抗蚀性能的评价因子，为喀斯特坡地水土流失治理中植被恢复措施的科学应用提供参考。选取重庆酉阳龙潭槽谷为研究区，分上、中、下坡分别布设拉巴豆和光叶苕子2种地埂篱，采用根系扫描仪和电子万能试验机测定其根系形态和力学参数，应变控制式直剪仪测定复合体抗剪强度，原状土冲刷水槽法测定复合体抗冲指数。结果表明：(1)抗剪复合体中，拉巴豆平均根长密度和根表面积密度分别高出光叶苕子59.32%和16.86%;抗冲复合体中，拉巴豆平均根长密度、根表面积密度和根体积密度较之光叶苕子高出30.48%、57.78%、92.98%;拉巴豆根系极限抗拉力和抗拉强度均显著高于光叶苕子。(2)2种地埂篱根系均能增强土壤的抗剪和抗冲性能，其中拉巴豆和光叶苕子复合体粘聚力较之对照土体分别增强了113.06%—124.37%和51.56%—87.12%,抗冲指数最高达到对照土体的2.81倍和2.45倍。(3)不同坡位，下坡2种植物的根长密度显著高于上、中坡；拉巴豆根系抗拉特性在下坡表现最优，光叶苕子在上坡表现更好；拉巴...     

不同护坡草本植物的根系特征及对土壤渗透性的影响

为明确三峡库区植被边坡植物物种根系特征与土壤渗透性之间的关系,以裸地为对照,应用WinRHIZO(Pro.2004c)根系分析系统对香根草(Vetiveria zizanioides(Lin.) Nash)、百喜草(Paspalum notatum Flugge)、狗牙根(Cynodon dactylon (L) Pers.)和紫花苜蓿(Medicago sativa L.)等4种护坡草本的根系特征进行定量分析.结果表明:(1)紫花苜蓿和香根草的根长密度和根表面积密度显著大于狗牙根和百喜草;(2)不同草本类型和同一草本不同土层之间土壤渗透性存在较大差异,且各草本土壤渗透性随土层深度的增加而降低;相对于裸地而言,4种草本均能显著增强土壤渗透性,其土壤渗透性优劣表现为:香根草＞紫花苜蓿＞百喜草＞狗牙根;(3)土壤的初始入渗率、稳渗率、平均渗透率和渗透总量等各参数均随根长密度和根表面积密度增大而增强,且与直径介于0.5-5 mm不同径级的根系特征之间存在明显的相关性,故根系对土壤渗透性的增强作用主要归功于0.5-5 mm径级的根长密度和根表面积密度;(4)根长密度、根表面积密度对考斯加科夫入渗模型参数K和a有较大影响,随着根长密度和根表面积密度的增加,表征土壤初始入渗率的K值逐渐增大,而表征入渗能力衰减的参数a逐渐减小.     

三江并流区水电站消落带适生草本植物根系固土能力

三江并流区生态脆弱敏感,水电站库周消落带土壤侵蚀严重,为研究消落带适生草本植物的根系固土效应,并为重建植被、控制土壤侵蚀提供依据,以生长期为18个月的风车草(Cyperus alternifolius L.)、美人蕉(Canna indica L.)、花叶芦竹(Arundo donax var. versicolor)和菖蒲(Acorus calamus L.)4种草本植物为研究对象,采用自制的原位剪切仪测定根土复合体和素土的抗剪强度;用根系拉力试验机测定根系的抗拉强度,用Wu和Waldron模型(WWM)对根系提高土体抗剪强度进行预测,并评价模型的可靠性。结果表明：①4种适生草本植物根系都能增强土体的抗剪强度,风车草、美人蕉、花叶芦竹和菖蒲根系使土体的抗剪强度分别提高了403.89%、248.32%、388.50%和200.71%;②4种草本植物根系的抗拉强度均与直径呈现负幂函数关系;③根系抗拉强度较大、破坏面上根面积比较高和根系直径(D)<1 mm细根较多的草本植物,固土效应更加显著;④4种草本植物根系对土体强度增量的WWM模型计算值是实测值的9.37-43.85倍,该模型对高含水率土壤中草本植物根系的预测精度较低。风车草、美人蕉、花叶芦竹和菖蒲的根系均有较强的固土能力,尤其是风车草和花叶芦竹,是三江并流区黄登水库消落带植被重建和固土抗蚀的优选物种。     

模拟氮沉降对中亚热带杉木幼树根系生物量的影响

植物根系是全球陆地生态系统碳储量的重要组成部分,在全球生态系统碳循环中起着重要作用,日益加剧的氮沉降会影响根系生物量在空间和不同径级的分配,进而影响森林生态系统的生产力和土壤养分循环。以杉木幼树为研究对象,通过野外氮沉降模拟实验,研究氮沉降四年后对不同土层、不同径级根系生物量的影响。结果发现：（1）低氮和高氮处理总细根生物量较对照均无显著差异（P > 0.05）,高氮处理粗根生物量及总根系生物量较对照分别增加45%和40%（P < 0.05）;（2）与对照相比,施氮处理显著增加20-40 cm与40-60 cm土层细根和粗根生物量,且在低氮处理下,20-40 cm土层细根、粗根在总土层细根与粗根生物量的占比显著提高。（3）与对照相比,高氮处理显著增加了2-5 mm、5-10 mm及10-20 mm径级的根系生物量,低氮处理显著增加2-5 mm、5-10 mm径级根系生物量,且显著降低20-50 mm径级根系生物量。综上所述表明：氮沉降后杉木幼树通过增加较粗径级根系来增加对养分及水分的输送,同时通过增加深层根系生物量及其比例的策略来维持杉木幼树的快速生长;而根系生物量的增加,在一定程度上会增加根系碳源的输入,影响土壤碳循环过程。     

绿竹根系分布及生物力学性质

为探讨绿竹根系固土力学机制,研究了绿竹根系在土壤中的垂直分布状况,以及绿竹单根抗拉强度和林地土壤抗剪切强度.结果表明:绿竹根系干质量、长度、表面积和体积均随土层深度增加而减小,0~40 cm土层集中了90%以上的根系.径级D≤1 mm根系占全部根系长度的比例最大,为79.6%,占全部根系体积的比例最小,为8.2%;而D≥2 mm根系则相反,D=1~2 mm根系居于二者中间.12%含水率和饱和含水率下,绿竹根系最大抗拉力与直径呈幂函数正相关,而根系抗拉强度与直径呈幂函数负相关;不同径级根系的抗拉强度存在显著差异,D≤1 mm根系抗拉强度最大,而D≥2 mm最小.12%含水率下根系抗拉强度显著高于饱和含水率下根系抗拉强度,含水率对根系抗拉强度的影响随根系径级增大而减小.绿竹林地土壤抗剪切强度和裸地土壤抗剪切强度均随土壤深度增加而增大.绿竹林地土壤抗剪切强度与根系含量呈线性正相关,且显著大于裸地土壤抗剪切强度,其增加值与根系含量呈指数正相关,而与土壤深度关系不大.     

浅层滑坡多发区典型灌木根系对边坡土体抗剪强度的影响

生态建设是"一带一路"可持续发展的基础,甘肃省陇南市位于"一带一路"核心区域,地处浅层滑坡多发区,地质灾害频发。通过单根抗拉试验和重塑土直接剪切试验对该区域四种典型灌木杠柳、胡枝子、酸枣和石榴的土壤及根系进行研究,探讨灌木根系对土壤物理性质和浅层滑坡的改善效应。结果表明,灌木根系能显著提高土壤含水率,改善孔隙结构;抗拉强度与根径间存在显著幂函数关系(P0.01),根径1 mm的毛细根抗拉强度最强,单根抗拉强度依次为胡枝子石榴酸枣杠柳;重塑土抗剪强度随土壤含水率升高而降低,土壤粘聚力(C)和内摩擦角(φ)均随含水率增加而减小,在10%的最优含水率下,抗剪强度依次为石榴酸枣杠柳胡枝子;随根系密度增加,杠柳和胡枝子的根-土复合体抗剪强度减小,酸枣和石榴在1.5倍天然根系密度下对土壤抗剪强度增强效果最强。通过评价浅层滑坡多发区不同灌木护土固坡效应,为"一带一路"沿线展开生态修复提供理论依据。     

壳聚糖对土壤栽培条件下烟草根系生长的影响

利用土培根箱装置,研究了0、20和40 mg·L~(-1)壳聚糖处理对广东南雄牛肝土、砂泥田土和紫色土中烟草根系生长随时间的变化。结果表明:根箱装置适用于观测3种植烟土壤中的根系动态生长;通过根箱观察面,发现壳聚糖处理显著增加了3种土壤中烟草根系的根长和根数,并且根长与根数的关系呈正相关;其中,在牛肝土和紫色土上,40 mg·L~(-1)壳聚糖处理效果较好,该处理提高了牛肝土上20~30和50~60 cm土层的总根长,以及紫色土上0~10和20~60 cm土层的总根长;而在砂泥田土上,20 mg·L~(-1)壳聚糖处理效果更优,该处理促进了10~40 cm土层根系的伸长;烟草在移栽后第24天,在20和40 mg·L~(-1)壳聚糖处理下,根长伸长率和根数增长率均出现了一个高峰,且显著高于对照处理。研究证明,壳聚糖对土壤栽培烟草根系生长具有促进作用。     

酸枣根系空间分布特征对自然干旱梯度生境的适应

以烟台、石家庄、银川和吐鲁番四个地区自然干旱梯度条件下生长的酸枣植株为试验材料,对酸枣根系的次生木质部导管及不同径级根系的分布特征进行研究。结果表明:从烟台到吐鲁番,酸枣根次生木质部中导管数量逐渐增多,管径依次增大。酸枣细根(d≤2 mm)长度远远大于其它径级根系的长度。随着干旱程度的增加,垂直方向上,细根出现在较深的土层,水平方向上,酸枣根幅扩大到560 cm,在末端或者接近末端的地方出现较多的细根分支。随着干旱程度的增加,5 mmd10 mm的根系长度在总根长中所占的比例逐渐增大,其可能为干旱生境中植株根系获取水分和养分的主要部位。不同生境中酸枣根系空间分布特征的变化是其长期生存于梯度干旱环境的适应特征。     

不同分类系统下油松幼苗根系特征的差异与联系

植物根序和径级不仅反映细根的形态结构, 而且能反映根系的一些生理特征, 如细根寿命和周转等。该文以二年生油松(Pinus tabulaeformis)幼苗根系为研究对象, 系统比较了根序分类方法和径级分类方法在描述根系特征上的优缺点, 探索了两者之间的内在联系。结果表明: 二年生油松幼苗最多可包括6级根序, 直径的变化范围为0.169-3.877 mm。按根序划分, I-VI级根序的总根长和总根表面积主要集中在前3级根序, 这3级根序的根占总根长的78.77%和总根表面积的62.72%。前3级根序的比根长是后3级根序比根长的1.3-3.0倍, 比根面积是后3级比根面积的1.0-1.5倍。按常用的径级(以0.5、1.0、1.5和2.0 mm为阈值)划分方法, 油松幼苗大部分根系直径≤1.5 mm, 此区间细根的根长和根表面积占总根长的93.76%和总根表面积的84.35%。直径≤1.5 mm的细根平均比根长是>1.5 mm细根比根长的3-7倍, 比根面积的1.5-3.0倍。由于油松根序和径级之间有显著的指数关系, 依据径级最大程度反映根序的原则, 提出了新的径级划分方法, 即以0.4、0.8、1.3和2.0 mm为阈值对油松幼苗根系径级重新进行划分。此时, 上述区间可分别包括I级、II级、III级、IV级、V级根序中根尖数的93.22%、86.37%、75.96%、70.47%和76.67%。同时也可分别涵盖各径级根长的89.34%-70.83%、根面积的86.01%-76.12%以及体积的87.73%-76.12%。此时, 根系不同径级与根序之间可以建立起良好的对应关系。这些结果表明, 通过合理划分径级区间可以较好地反映根序 特征。     

A parametric distribution for the fraction of outdoor soil in indoor dust

For a chemical that does not have a source inside a house, the ratio of its dust concentration indoors to its soil concentration outdoors is equal to the fraction of house dust that is composed of soil. To estimate the fraction of soil in house dust, we compiled ratios of the concentrations of a chemical in dust and soil from the scientific literature. We find that a lognormal distribution fits the data extremely well. This distribution is suitable for use in public health risk assessments for single‐family homes in temperate climates.     

黄土和风沙土藓结皮土壤呼吸对模拟降雨的响应

生物结皮土壤呼吸是干旱和半干旱生态系统碳循环的重要组成部分,但目前其对降雨的响应规律尚不明确。针对黄土高原黄土和风沙土上发育的藓结皮,分别进行2、4、6、10、20、30、40 mm的模拟降雨,并使用便携式土壤碳通量分析仪测定雨前和雨后藓结皮的呼吸速率,对比分析降雨量对藓结皮呼吸速率的影响;同时,在40 mm降雨后的0—24 h连续测定藓结皮的呼吸速率变化,分析藓结皮呼吸速率随雨后历时的变化规律。结果显示,7种降雨量后两种土壤上藓结皮的呼吸速率均显著升高,黄土上藓结皮呼吸速度的增幅为2.89—6.38倍,风沙土上藓结皮呼吸速率的增幅为0.73—4.38倍。0—6 mm降雨中,两种土壤上藓结皮的呼吸速率均随降雨量增加而迅速升高,二者成显著线性正相关关系;6—40 mm降雨中,黄土上藓结皮的呼吸速率随降雨量增加而缓慢升高,但风沙土上藓结皮的呼吸速率随降雨量增加而快速降低。两种土壤上藓结皮的呼吸速率随雨后历时表现出相似的变化规律,即雨后迅速升高、之后逐渐降低,并在24 h左右回归到雨前水平;但黄土上藓结皮的呼吸速率在雨后即刻达到峰值,而风沙土上藓结皮的呼吸速率在雨后30 min左右方达到峰值。黄土上藓结皮的呼吸速率一致高于风沙土上的藓结皮,前者在不同降雨量和雨后历时中平均比后者高150.0%和59.6%。此外,藓结皮呼吸速率与表层土壤含水量存有显著相关关系,在含水量较低(小于约4%)时二者显著正相关,在含水量较高(大于约4%)时二者对于黄土上藓结皮为正相关、对于风沙土上藓结皮为负相关。研究表明,黄土高原藓结皮土壤呼吸对降雨响应快速而直接,但其响应规律对于黄土和风沙土上的藓结皮是不同的,总体而言黄土上藓结皮对降雨的响应更为持久有效。     

渭北旱塬苹果园土壤紧实化现状及成因

本研究通过分析渭北旱塬苹果园土壤的紧实化现状及其诱导因素,找出影响当地苹果园健康发展的土壤退化隐性因素,为果园科学管理提供理论依据。分别选取种植年限＜10年(4～6年)、10～20年(14～16年)和＞20年(24～26年)的苹果园各4个,分析0～60 cm土层土壤容重和紧实度随土层深度的变化规律,探明果园土壤内部紧实化发生的部位和退化程度,同时,通过分析土壤团聚体数量及其稳定性、土壤黏粒和有机质含量,揭示引起渭北果园土壤内部紧实化的原因。结果表明: 渭北果园0～60 cm土层土壤容重和紧实度均随植果年限和土层深度的增加而显著增大。以20 cm土层为界,渭北各园龄段苹果园土壤具有明显的“上松下实”变异特征,20 cm以上土层上述各指标基本满足苹果树的正常生长需求,20 cm以下土层土壤则已超出了苹果树健康生长的阈值。造成渭北苹果园亚表层以下土壤紧实化的原因主要是土壤团聚作用差、有机质含量低,加之植果期间人为扰动少,土壤中分散的黏粒会向下层移动。此外,随着植果年限的增加,土壤紧实化过程更加明显。     

Various Applications of Soil Contaminant Database Developed for the Central Artery/Tunnel Project

One of the largest environmental assessment programs in the United States was initiated in the early 1990s to determine the chemical characteristics of soil located within the planned alignment for the Central Artery (I-93) / Tunnel (I-90) (CA/T) Project in Boston, Massachusetts. The primary purpose of the program was to support management of the handling and disposal of over 17 million cubic yards of soil to be excavated during construction of the CA/T Project. As part of this work, more than 8,000 soil samples were collected from more than 2,600 soil borings and analyzed for a range of chemical contaminants, including volatile organic compounds, acid/base neutral compounds, total petroleum hydrocarbons, polychlorinated biphenyls, and heavy metals. The soils encountered during the investigations exhibited properties influenced by numerous anthropogenic activities. These activities, such as vehicular emissions, historic industrial/manufacturing operations, and waterfront filling with both building rubble and dredge spoils from Boston Harbor, resulted in soils primarily contaminated with petroleum hydrocarbons and metals. As a result of this program, an extensive database of the chemical constituents present in urban soils in downtown Boston was developed. These results were primarily used to delineate the limits of contaminated areas affecting the planned construction. In addition, the database has been used by the Project to support various soil management activities, as well as by the regulatory community in developing guidelines and criteria governing the management of contaminated soils in Massachusetts. This paper focuses on the various applications of this database throughout the course of the Project, and with the additional aim of stimulating potential future applications by both the regulatory and scientific communities.     

恩诺沙星残留对土壤微生物功能的影响

研究了恩诺沙星残留对土壤呼吸作用、纤维分解作用、氨化作用、硝化作用的影响 ,结果表明 ,相对较低浓度恩诺沙星残留(0 .0 1μg/ g土 ,0 .1μg/ g土 )刺激土壤呼吸作用 ,相对较高浓度恩诺沙星残留 (1μg/ g土 )对土壤呼吸作用产生抑制 ,药物作用活性维持期为 6 d;恩诺沙星残留对土壤纤维分解作用影响较不明显 ;较低浓度恩诺沙星残留 (0 .0 1μg/ g土 ,0 .1μg/ g土 )对土壤氨化作用有刺激作用 ,而较高浓度恩诺沙星残留 (1μg/ g土 ,10μg/ g土 )则会对其起抑制作用 ,药物作用活性期为 9d;不同浓度恩诺沙星对土壤硝化作用影响极其显著 ,当恩诺沙星浓度达到 1μg/ ml时 ,在 3～ 9d内 ,对土壤硝化作用有一定抑制作用。当恩诺沙星浓度达到 10μg/ ml时 ,强烈抑制了土壤硝化作用 ,直到本试验结束时 ,其抑制作用未见减弱。结果表明恩诺沙星残留影响了土壤微生物这些功能 ,因而可能影响到土壤特性和土壤中一些生态过程     

Concept,Components, and Strategies of Soil Health in Agroecosystems

The terms ''''soil health'''' or ''''soil quality'''' as applied to agroecosystems refer to the ability of soil to support and sustain crop growth while maintaining environmental quality. High-quality soils have the following characteristics: (i) a sufficient, but not excess, supply of nutrients; (ii) good structure (tilth); (iii) sufficient depth for rooting and drainage; (iv) good internal drainage; (v) low populations of plant disease and parasitic organisms; (vi) high populations of organisms that promote plant growth; (vii) low weed pressure; (viii) no chemicals that might harm the plant; (ix) resistance to being degraded; and (x) resilience following an episode of degradation. Management intended to improve soil health involves creatively combining a number of practices that enhance the soil''s biological, chemical, and physical suitability for crop production. The most important general strategy is to add plentiful quantities of organic matter—including crop and cover crop residues, manures, and composts. Other important strategies include better crop rotations, reducing tillage and keeping the soil surface covered with living and dead residue, reducing compaction by decreasing heavy equipment traffic, and using best nutrient management practices. Practices that enhance soil quality frequently reduce plant pest pressures.     

不同地表覆盖方式对苹果园土壤性状及果树生长和产量的影响

以黄土高原9年生红富士果园生态系统为对象,研究不同地表覆盖模式（清耕、生草覆盖、地膜覆盖、秸秆覆盖和砂石覆盖）对果园土壤性状及果树生长和产量的影响.结果表明：生草覆盖土壤水分剖面分异最低,砂石覆盖土壤水分剖面分异最高;砂石覆盖提高了根层水分含量,有利于果树对水分的利用.不同地表覆盖模式土壤热量状况变化显著,处理间差异明显,极端最高温度下降,但地膜覆盖处理夏季地温超过果树根系生长的上限温度,对果树根系生长和生理功能发挥不利.除地膜覆盖外,其他地表覆盖模式均能提高土壤CO₂释放速率,其中生草覆盖的效果最为显著.不同地表覆盖模式对果树枝条类型比例及产量影响较大,砂石覆盖处理的中短枝比例和果实产量最高;生草覆盖处理的果实产量最低.因子分析结果表明,对于黄土高原沟壑区盛果期果园,砂石覆盖处理是较为适宜的地表覆盖模式.     

A rapid,cost-effective procedure for the extraction of microbial DNA from soil

Here we describe a DNA extraction method that is based on a simple, rapid polyvinylpolypyrrolidone–calcium chloride precipitation to release microorganisms from the soil combined with lysozyme–proteinase–SDS lysis of the microbial community. The extracted DNA is of high quality and allows direct detection of specific genes by the polymerase chain reaction (PCR) as well as cloning of indigenous microbial DNA. This method facilitates the extraction of 36 500-mg soil samples simultaneously in a 2-h period by one person. The procedure is safe, inexpensive, and does not require specialized equipment or generate hazardous wastes.     

Trajectories of change: riparian vegetation and soil conditions following livestock removal and replanting

Riparian zones provide critically important ecological functions, including the interception of nutrients and sediments before they enter waterways. Consequently, riparian zones, and the vegetation they support, are often considered as an important ‘final buffer’ between waterways and adjacent land. In agricultural ecosystems, riparian zones are therefore increasingly recognized as an important component of strategies aimed at minimizing the flow of nutrients and sediments into waterways. Accordingly, riparian zones are increasingly afforded protection and are targeted for restoration. Here we present results of a study in which we aimed to identify patterns of change in soil and vegetation properties in riparian zones, under different management regimes, adjacent to tributary streams in one of south‐eastern Australia's main agricultural regions. We compared riparia that were heavily impacted by agricultural activities, were in remnant condition or had undergone some restoration activities and were thus in a transitional state. There was an increase in plant cover and soil C concentration between impacted through to remnant sites, with transitional sites intermediate, suggesting that improvements in soil conditions were becoming evident following restoration activities. In our assessment of soil physicochemical properties we investigated the relationships between riparian condition and soil properties, taking into account the influence of adjacent land use on these relationships. Importantly, the concentrations of NO₃^‐ and plant available P in riparian surface soils were more or less influenced by concentrations in the adjacent land depending upon riparian condition. This will, in turn, have consequences for nutrient inputs into streams. This study emphasizes that riparian zones need to be managed within their wider landscape context. Furthermore, the results of this study will inform efforts seeking to minimize impacts of agricultural activities on waterways, through the conservation and/or restoration of riparian ecosystems.     

土壤微生物资源管理、应用技术与学科展望

土壤中蕴藏着高度的微生物多样性,在陆地生态系统中发挥着非常重要的功能,加强对土壤微生物资源的综合管理与开发应用是提升生态系统稳定性与生产力及农产品质量的重要途径。首先,土壤微生物多样性具有全球性的重大意义,有待完善对土壤微生物的检测与监测技术研究,进而实现土壤微生物多样性与土壤功能的耦合以及对土壤质量的评定;其次,土壤微生物作为一种宝贵的生产资料和可持续资源,要加强其在土壤肥力强化与保育、土壤障碍消减与调节、土壤污染控制与修复等3个领域的应用研究。最后,未来土壤微生物学发展将会形成土壤微生物系统学、土壤微生物过程学与土壤微生物功能学3个子学科,要建立土壤微生物种质资源库与遗传信息库,推进土壤微生物生理代谢过程、生物化学过程及生态行为过程的研究,联结土壤微生物与土壤功能的关系,并从土壤中的功能微生物出发对环境变化作出积极响应和主动调控。此外,原创性方法的建立与应用是限制土壤微生物学发展的技术瓶颈,联合生物地理学与生物信息学破译重要基因的特定生态功能,并将其应用到生态模型以及生态系统未知领域的研究中去,是土壤微生物学面临的挑战。