Approximate analytical solutions of root surface nutrient uptake flux and rhizosphere solute concentrations

该文用Nye-Tinker-Barber模型来研究植物根系表面的养分吸收通量和根围溶质浓度的近似解析解。将根围区域分为远场区域和近场区域, 在远场用相似变量, 在近场用尺度变换, 将远场解在根表面展开并与近场解进行待定函数的匹配, 从而获得对流扩散方程根表面通量和浓度的一阶近似解析解, 该解能够简化到扩散方程的解的形式。对氮、钾、硫、磷、镁、钙的养分吸收通量和氮、钾的浓度分别进行数值模拟, 比较模型的数值解、Roose的近似解析解和该文的近似解析解。结果表明: 在扩散方程中, 6种元素通量的解析解与Roose解析解相近, 但均高于数值解, 钾和磷的通量在短时间内迅速衰减; 钾和氮浓度的全局近似解析解与Roose解析解接近, 并与数值解的变化趋势一致。在对流扩散方程中, 除氮外的5种元素通量的近似解较Roose的解析解更接近于数值解, 且没有奇性。     

氮肥对夏秋季茶树吸收根生物量和养分储量的影响

以12年生龙井43茶树为研究对象,在7月至翌年1月利用土钻法对连续5a施用不同氮肥处理后的茶树吸收根生物量和养分含量进行了研究。结果表明茶树吸收根生物量在0.34-0.72 mg/dm3之间,碳、氮、磷、钾和镁储量变异范围分别为12.6-25.2 mg/dm~3、4.55-11.2 mg/dm~3、0.47-1.19 mg/dm~3、1.31-4.05 mg/dm~3、0.30-1.19 mg/dm~3。茶树吸收根生物量和各养分含量随月份变化呈现双峰型,峰值分别在8月和翌年1月,而7月和11月生物量和养分储量均较低。与不施肥对照相比,施用氮肥影响茶树吸收根生物量,氮肥施用对茶树吸收根生物量的影响因氮肥施用时间而异。不同氮肥施用水平下茶树吸收根总碳浓度和总碳含量均不存在显著差异。受氮肥施用时间影响,施氮对茶树吸收根氮浓度的影响不同月份间存在差异,其中7月、8月和1月施氮处理下氮浓度较高,而9月、10月和11月不施氮处理下氮浓度较高。氮肥施用对各月份茶树吸收根氮养分储量均没有显著影响。氮肥施用降低了部分月份茶树吸收根磷、钾和镁的浓度和储量。施用中等用量的氮肥能缩小茶树吸收根夏秋季氮磷钾镁养分储量的月份间差异。     

不同施肥条件下毛叶苕子的腐解及养分释放特征

利用田间埋袋法,研究不施肥、施氮肥、施石灰3种处理对豫南稻田毛叶苕子腐解及养分释放特征的影响.结果表明:不同施肥处理下毛叶苕子累积腐解率为65.3%~72.5%,腐解过程中呈现前11 d腐解较快、后期腐解缓慢并逐渐趋于平稳的趋势.不同处理养分释放率表现为钾>磷>碳>氮,试验结束时(翻压148 d),碳、氮、磷、钾的累积释放率分别为83.6%~84.6%、78.2%~81.2%、89.8%~91.4%、96.3%~97.0%.在整个腐解期内,毛叶苕子氮释放特征与腐解特征相似,与不施肥相比,施石灰促进毛叶苕子腐解及氮、磷、钾养分释放;施氮肥促进毛叶苕子磷释放,抑制钾释放;施石灰和氮肥对碳释放均无显著影响.施氮肥处理腐解0~11 d促进毛叶苕子腐解及氮释放,腐解11~148 d抑制毛叶苕子腐解及氮释放.采用一级动力学方程及对数函数方程拟合豫南稻区毛叶苕子腐解及碳、氮、磷、钾养分释放特征均达到显著水平,拟合方程的特征参数值与毛叶苕子腐解率及养分释放率呈显著相关.施用石灰促进毛叶苕子腐解及养分释放的效果优于施用氮肥;一级动力学方程及对数函数方程特征参数值可较好地描述毛叶苕子腐解及养分释放能力.     

Shifts in chemical and microbiological properties belowground of invader Ageratina adenophora along an altitudinal gradient

入侵植物紫茎泽兰根围土壤化学及微生物属性海拔变化格局 热带地区山地生态系统是外来植物入侵的重要区域,是研究外来植物扩散机制的“天然实验室”。本研究试图探明入侵植物紫茎泽兰(Ageratina adenophora)根围土壤化学(pH及土壤养分)和微生物(酶活性和细菌群落)特性沿海拔梯度的变化规律。本研究以哀牢山(1400–2400 m)不同海拔梯度分布的紫茎泽兰为研究对象,采集根围土,测定土壤有机碳及养分含量,以及植物根系碳和氮含量。分析与土壤有机碳、氮及磷循环的酶活性,通过计算土壤酶化学计量参数,探究微生物生长代谢利用碳、氮及磷的规律。借助高通量测序技术对16S rDNA的V4区测序,分析细菌群落结构。研究结果显示,海拔显著影响紫茎泽兰根系氮及及其根围土壤有机碳含量,且这些测量指标在海拔2000 m  出现拐点。处在低海拔,入侵植物快速生长耗竭土壤中相对缺乏的磷,磷素是限制微生物生长的重要养分元素;而在高海拔,微生物需要投入更多的能量降解有机质获取碳,导致微生物生长的碳限制。细菌群落β多样性及pH  是决定不同海拔酶化学计量参数差异的重要因子;变形菌门和酸杆菌门是决定微生物养分利用状况的主要细菌门类。这些结果阐明了不同海拔梯度上紫茎泽兰根围土壤微生物的养分利用规律,有助于认识入侵植物沿海拔扩散机制。     

人工油松林的化学元素特征

28年生人工油松林的建群种——油松各器官化学元素浓度由叶、小枝、枝和树干逐渐下降。叶内元素浓度高低,以碳、氮、钙、钾、镁、磷为序。地下部分细根较粗根的元素浓度为大。灌木的化学元素的共同特点是碳含量最高,其次为氮、钾和钙。灌木叶片中的元素浓度大于茎。草本植物地上部分元素浓度明显低于灌木叶。灌木根系内化学元素浓度均低于它的地上部分。枯枝落叶的化学成分与活的枝、叶相比,铁的浓度显著增加,其次为铝,其他元素的浓度或多或少有所下降。在人工油松林各层次植物中,以碳素积累量最高,其次为钙和氮。元素的存留量仍以碳素为高,其次在乔木层中存留量以钙较大,在灌木层中以氮、钾较高。元素的年归还量除碳以外,钙较高,钾、磷较低。人工林的吸收量/土壤贮量的比值,以钾和磷较高。土壤中代换性钾、磷的贮量相对不大,为促进人工林生长,增施磷肥和钾肥将是有效的。     

基于GIS的缓坡烟田土壤养分空间变异研究

综合运用地统计学和GIS相结合的方法,分析了缓坡地形下土壤养分的空间变异规律,并绘制养分空间分布图,为山地缓坡烟田养分分区及精准施肥决策提供理论依据.结果表明:研究区内4种养分含量均具中等程度变异.土壤有机质、碱解氮、速效磷和速效钾的变程分别为61.8、76.3、70.5 m和57 m.土壤速效钾的分形维数最高,有机质和碱解氮其次,速效磷最低.有机质和速效钾的最适模型为指数模型,块金系数分别为30.9％和31.1％;碱解氮和速效磷可用球状模型进行较好拟合,其块金系数分别为37.7％和26.4％,4种养分均有中等程度的空间相关性.各向异性和趋势性分析均显示,有机质和速效磷具有较强的各向异性,碱解氮和速效钾的各向同性范围最广.研究区4种养分的空间分布格局在海拔和坡度的影响下呈现出一定的规律性,低值均在坡度较大的中北部出现,东北部和南部较平缓区域出现高值.     

木薯/花生间作对根际土壤微生态的影响

为了探明木薯/花生间作在增产增收的同时对土壤微生态的影响,研究木薯和花生以不同行距(30 cm,40 cm,50 cm)间作的根际土壤养分、微生物及相关酶活性的变化。结果表明:木薯/花生间作可增加根际土壤细菌、真菌、放线菌及总微生物数量和微生物多样性,30 cm间作行距的木薯、花生根际土壤微生物总数量分别比单作木薯、花生增加了129.6%和101.1%;间作根际土壤碱解氮、有效磷、有效钾和有机质含量相比单作增加,50 cm间作花生的根际土壤碱解氮、有效磷、有效钾量比单作花生增加了145.9%~195.9%,30 cm间作木薯的根际土壤有效钾、有效磷含量分别比单作木薯增加了161.8%和187.9%;木薯/花生间作的根际土壤过氧化氢酶、酸性磷酸酶活性活性相比单作升高,间作土壤脲酶和蛋白酶活性相比单作降低,30 cm间作木薯的根际土壤过氧化氢酶活性比单作木薯增加了59.2%,50 cm间作花生的根际土壤蔗糖酶活性比单作花生增加了97.4%。可见,木薯/花生间作可改善根际土壤微生态坏境,且适宜的间作行距更利于土壤养分含量和微生物数量的增加。     

花粒期光照对夏玉米干物质积累和养分吸收的影响

选用登海605(DH605)为试验材料,在大田条件下通过花粒期遮阴(S)和增光(L)研究不同光照对花后夏玉米产量、干物质积累和氮、磷、钾养分吸收与运转特性的影响.结果表明: 遮阴后夏玉米产量、干物质积累量及氮、磷、钾养分吸收量均显著降低;而增光有利于夏玉米干物质积累量及氮、磷、钾养分吸收量和产量的提高.2011-2013年,遮阴处理的产量较对照(自然光下)分别降低了59.4%、79.0%、60.6%;增光后产量分别增加16.3%、12.9%、6.8%.遮阴对干物质积累的影响大于其对植株氮、磷吸收量的影响,植株体内氮、磷等养分含量有所上升,而钾吸收量的下降幅度大于干物质积累,钾素相对含量降低,氮、磷、钾向籽粒的分配比例降低.增光后干物质积累和氮、磷吸收量显著上升,但对氮、磷吸收的影响更大;增光条件下,氮、磷、钾等养分向籽粒的分配比例增加.
     

半夏测土配方施肥产量效应和氮磷钾吸收特性分析

目的：探索肥效对贵州半夏产量及养分吸收特性的影响。方法：采用“3414”测土配方施肥考察半夏产量及不同时期块茎对氮磷钾吸收特性,SPSS 22.0进行肥效方程拟合及不同时期块茎氮磷钾吸收的显著性分析。结果：氮、磷、钾肥施用量的变化对半夏产量具有显著相关性,通过对氮、磷、钾肥施用量与半夏产量的关系拟合得到单因素肥效方程、三因素肥效模型以及不同时期块茎吸收氮磷钾与产量的相关性模型,该区域半夏最佳施肥策略为氮肥74.19 kg/hm²、磷肥87.28 kg/hm²、钾肥25.48 kg/hm²;不同时期块茎对氮的吸收受磷肥施用的影响,当磷肥施用处于较高水平时,块茎对氮的吸收也处于较高水平;块茎对磷的吸收受钾肥施用的影响,当钾肥施用处于较低水平时,对磷的吸收处于较高水平;块茎对钾的吸收则受氮、磷施用的共同影响,高钾的施用有利于块茎对钾的吸收。结论：半夏不同生长期应采取不同的施肥策略以达到更高的产量,本研究对贵州半夏高产栽培有一定指导意义。     

艾比湖流域小尺度农田土壤养分的空间分布和盐渍化风险评价

为了解绿洲经济迅速发展背景下新疆典型尾闾绿洲-艾比湖流域小尺度农田土壤的养分和盐渍化状况,对该地区典型农田土壤中有机质、碱解氮、速效磷和速效钾等养分元素的空间分布、影响因素以及盐渍化风险状况进行了评价。结果表明:(1)农田土壤中有机质、碱解氮、速效磷和速效钾的含量均较高。所有土壤样点中总盐分含量属于高度变异,其他指标属于低度变异。(2)半方差函数分析表明土壤中碱解氮、速效磷和速效钾含量的空间变异性主要受施肥和灌溉等随机性因素的影响;而有机质和总盐分含量的空间变异性则受植被覆盖和土壤质地等结构性因素以及施肥、灌溉等随机性因素的共同影响。(3)空间分析表明,总体看农田土壤中有机质、碱解氮、速效磷和速效钾含量较高区域主要分布在中部和北部,受施肥、灌溉方式和植被盖度等因素的影响;而盐分含量较高区域主要分布在研究区南部和边缘区域,主要受地形、土壤质地和植被盖度的影响。(4)相关分析表明农田土壤中有机质、速效钾、速效磷、碱解氮和总盐分含量呈显著的负相关关系。盐渍化风险评估表明土壤中总盐分含量属于低度到中度的盐渍化风险,不会对主要作物棉花的生长产生危害,但应改进灌溉方式和种植制度,同时采用增施有机肥、进行秸秆还田等措施促进棉花作物的稳产、高产。     

Measured and modelled differences in nutrient concentrations between rhizosphere and bulk soil in a Norway spruce stand

The gradient in soil characteristics from the bulk soil to the root surface is important to roots and to the organisms that live in the rhizosphere. Our ability to measure ion concentrations at the root surface is extremely limited, and models are largely untested. We used data from a well studied Norway spruce stand in SW Sweden to compare the measured difference in nutrient concentrations between rhizosphere and bulk soil with the difference predicted by a steady-state simulation model based on ecosystem budgets of nutrient uptake. The simulation model predicted depletion of NH₄, Ca, Mg, K in the rhizosphere, which shows that budgeted uptake rates were greater than the mass flow of bulk solution towards the root. In plots treated with ammonium sulphate, the model predicted an accumulation of S in the rhizosphere. In contrast, the observed rhizosphere concentrations were generally enriched in nutrients, relative to bulk soil. Collecting rhizosphere soil adhering to root surfaces may not be an appropriate method for describing the concentration gradient around the root. In addition, the simulation model omits some processes affecting conditions in the rhizosphere that are important to explaining nutrient uptake.     

Nutrient composition of Douglas-fir rhizosphere and bulk soil solutions

Rhizosphere soil solution is the direct source of nutrients for plant uptake. The nutrient composition of rhizosphere soil solution can be very different from that of bulk soil solution due to root exudation, nutrient uptake and rhizosphere microorganism activity. This study examined the nutrient composition of Douglas-fir rhizosphere soil solution in two soils belonging to the Nisqually and Pitcher soil series and compared rhizosphere solution with that of bulk soil solution. Fertilized and unfertilized Nisqually soils were also compared. Soil solutions were collected using centrifugation. Results indicated that nutrient concentrations in the rhizosphere solutions were typically higher than that of bulk soil solutions when no fertilizer was applied. Differences in the concentrations of nutrients between the rhizosphere and bulk soil solutions were masked by the addition of fertilizers. Rhizosphere solution pH also appeared to be affected by the concentration of NH₄ and NO₃ in the solution. With a higher concentration of NH₄ relative to NO₃ in the rhizosphere soil solution, the solution pH of the rhizosphere was lower than that of the bulk soil, but with a lower concentration of NH₄ relative to NO₃, the solution pH of the rhizosphere was higher than that of the bulk soil solution.     

Gradients in soil solution composition between bulk soil and rhizosphere – In situ measurement with changing soil water content

Soil solution composition changes with time and distance from the root surface as a result of mass flow, diffusion, plant nutrient uptake and root exudation. A model system was designed, consisting of a root compartment separated from the bulk soil compartment by a nylon net (30 m mesh size), which enabled independent measurements of the change of soil solution composition and soil water content with increasing distance from the root surface (nylon net). K⁺ concentration in the rhizosphere soil solution decreased during the initial growth stage (12 days after planting, DAP). Thereafter K⁺ accumulated with time, due to mass flow as the dominating process. The extend of K⁺ accumulation depended on the initial fertiliser application. As K⁺ concentrations in soil solution increase, not only as a result of transport exceeding uptake, but also as a result of decreasing soil water content, it is hypothesised that K concentration in soil solution is not the only trigger for the activity of K transporters in membranes, but ABA accumulation in roots induced by decreasing soil matric potentials may add to the regulation. A strong decrease of rhizosphere pH with time is observed as a result of H⁺ efflux from the roots in order to maintain cation-anion balance. In addition the K⁺ to Ca²⁺ ratio was altered continuously during the growing period, which has an impact on Ca²⁺ uptake and thus firmness of cell walls, apoplast pH, membrane integrity and activity of membrane transporters. The value of osmotic potential in the rhizosphere soil solution increased with time indicating decreasing soil water availability. Modelling approaches based on the data obtained with the system might help to fill in the time gaps caused by the low temporal resolution of soil solution sampling method.     

摩西斗管囊霉改善连作花生根际土壤的微环境

花生(Arachis hypogaea)长期连作导致土壤环境恶化, 严重影响产量和品质。丛枝菌根真菌(AMF)作为有益真菌能够与80%的陆生植物根系形成共生关系, 这种共生体能够改善植物根系微环境, 提高植物对营养物质的吸收和对逆境胁迫的抗性。为了探究AMF对花生连作土壤微环境的影响, 该研究通过对花生连作土壤接种和未接种摩西斗管囊霉(Funneliformis mosseae)试验, 在花生不同生长期检测根际土壤的酶活性、土壤矿物质含量、土壤微生物群落结构和多度的变化情况, 以及对连作花生产量和品质的影响。研究结果表明: 1)摩西斗管囊霉能够显著提高花生根际土壤蔗糖酶、脲酶、碱性磷酸酶和硝酸还原酶的活性; 2)摩西斗管囊霉显著增加花生连作土壤中全氮、全磷、全钾、速效磷和速效钾的含量; 3)摩西斗管囊霉显著降低土壤中有害真菌曲霉菌属(Aspergillus)的多度, 减少镰刀菌属(Fusarium)和赤霉菌属(Gibberella)的多度, 但是没有达到显著水平, 显著增加有益细菌放线菌Gaiella属的多度; 4)摩西斗管囊霉显著提高连作花生的产量, 增加籽仁中蛋白质、油酸和亚油酸的含量。因此, 摩西斗管囊霉能够改善连作花生根际土壤微生态环境, 增强连作土壤对致病菌的抵抗能力, 从而缓解连作障碍对花生根系的危害。     

Genotypic effects in phytoavailability of radiocaesium are pronounced at low K intensities in soil

The differences in radiocaesium uptake between species were analysed in a series of solution culture and pot trials. Since radiocaesium uptake is very sensitive to the solution potassium (K) concentration, it was hypothesised that species depleting K in the rhizosphere to a larger extent, will have a higher radiocaesium uptake. Five species (bean, lettuce, winter barley, ryegrass and bentgrass) were grown for 18–21 days in nutrient solution spiked with ¹³⁷Cs and at 4 K concentrations between 0.025 and 1.0 mM. Shoot ¹³⁷Cs activities all decreased between 17- and 81-fold with increasing K supply. Shoot ¹³⁷Cs activities were 4-fold different between species at the lowest K supply and 3.4-fold different at high K supply. The same five species were grown in two ¹³⁴Cs spiked soils with contrasting exchangeable K but similar clay content. Shoot ¹³⁴Cs activities were up to 19-fold higher in the soil with lowest exchangeable K. Differences in shoot activity concentrations between the species were only 4.5-fold in the high K soil, but were 15-fold in the low K soil. Bulk soil solution ¹³⁴Cs and K concentration data were combined with radiocaesium uptake characteristics measured in solution culture to predict radiocaesium uptake from soil. Predictions were within 1.6-fold of observations in the high K soil but largely underestimated ¹³⁴Cs uptake in lettuce, ryegrass and barley in the low K soil. A solute transport model was used to estimate K and radiocaesium concentrations in the rhizosphere. These calculations confirmed the assumption that higher radiocaesium uptake is found for species that deplete K in the rhizosphere to a larger extent.     

Influx and efflux of amino acids from Zea mays L. roots and their implications for N nutrition and the rhizosphere

The aim of the study was to investigate the ability of Zea mays L. roots to regulate the amount of free amino acids present in the rhizosphere. The active uptake of amino acids was shown to conform to Michaelis-Menten kinetics. Comparison of amino acid-N and NO₃-N kinetic parameters and soil solution concentrations showed that root uptake of free amino acids from soil may contribute significantly to a plant's N budget. The influx of amino acids also helps to minimize net C/N losses to the soil, and is therefore important in regulating the size of the rhizosphere microbial population. Experimental data and a computer simulation model of amino acid influx/efflux in a sterile solution culture, showed that roots were capable of re-sorping over 90% of the amino acids previously lost into solution as a result of passive diffusion.     

Soil solution chemistry in the rhizosphere of roots of sessile oak (Quercus petraea) as influenced by lime

This study describes the soil solution chemistry in the rhizosphere of fine roots of sessile oak ( Quercus petraea (M.) Liebl.) grown in rhizotrons. A control was compared with soils treated with an equivalent CaCO₃ of 1.4 t ha^-1 CaO. Solution samples were extracted from the B-horizon using micro suction cups with a suction of _∼40 kPa. Two series of experiments were carried out: one irrigated with rain water (age of seedling 2 to 4 months) and one irrigated with demineralized water (age of seedlings 1.5 to 2 months). Half of the sampling points were choosen close to the roots and half in the bulk soil. In both experiments there was generally no rhizospheric gradient after liming. In contrast, in the control, depletion in the rhizosphere occurred for most of the ions studied (Mg, Ca, Al, K, NO₃ ^-, NH₄ ⁺, Cl^-) in the demineralized water experiment, but this was different when rainwater was used. The latter effect is probably due to the higher solution concentrations in the rainwater experiment but could also be a result of root damage due to low Ca/Al ratios in the rhizosphere solution. It was concluded, that liming improved the chemical composition in the rhizosphere soil solution by increasing overall solute concentration to levels enabling sufficient and easier nutrient uptake by roots. This revised version was published online in June 2006 with corrections to the Cover Date.     

Effects of short-term nitrogen addition on fine root biomass,lifespan and morphology of Castanopsis platyacantha in a subtropical secondary evergreen broad-leaved forest

Aims Fine roots are the principal parts for plant nutrients acquisition and play an important role in the underground ecosystem. Increased nitrogen (N) deposition has changed the soil environment and thus has a potential influence on fine roots. The purpose of this study is to reveal the effect of N deposition on biomass, lifespan and morphology of fine root.Methods A field N addition experiment was conducted in a secondary broad-leaved forest in subtropical China from May 2013 to September 2015. Three levels of N treatments: CK (no N added), LN (5 g·m^-2·a^-1), and HN (15 g·m^-2·a^-1) were applied monthly. Responses of fine root biomass, lifespan, and morphology of Castanopsis platyacantha to N addition were analyzed by using a minirhizotron image system from April 2014 to September 2015. Surface soil sample (0-10 cm) was collected in November 2014 and soil pH value, and concentrations of NH₄⁺-N and NO₃^--N were measured.Important findings The biomass and average lifespan of the fine roots of C. platyacantha were 128.30 g·m^-3 and 113-186 days, respectively, in 0-45 cm soil layer. Nitrogen addition had no significant effect on either fine root biomass or lifespan in 0-45 cm soil layer. However, LN treatment significantly decreased C. platyacantha root superficial area in 0-15 cm soil layer. HN treatment significantly decreased soil pH value. Our study indicated that short-term N addition influences soil inorganic N concentration and thus decreased pH value in surface soil, and thereafter affect fine root morphology. Short-term N addition, however, did not affect the fine root biomass, lifespan and morphology in subsoil.