Mobilization of aluminium in the rhizosphere soil solution of growing tree roots in an acidic soil

Chemical conditions in the rhizosphere in many respects are different from the bulk soil. Especially in acid forest soils aluminium chemistry at the soil root interface is of particular interest because of its importance for evaluating the risk of rhizotoxicity. In the present study we have used micro suction cups to collect soil solution from the rhizosphere of oak seedlings (Quercus robur L.) in high spatial resolution and capillary electrophoresis for the determination of major ions and Al³⁺. While the concentrations of nutrient cations, especially Ca²⁺ and Mg²⁺, decreased in the vicinity of growing roots the concentrations of Al³⁺ significantly increased. Al³⁺-ions were probably released when root-exuded protons were buffered by the soil. Their occurrence indicates, that the oak roots in our experiments had only limited capabilities to detoxify Al in their rhizosphere. The restriction of this effect to the very small soil compartment close to the roots suggests, that common soil analysis which neglect rhizosphere processes might greatly underestimate the in situ concentration of Al³⁺ near tree roots. Our experiments furthermore indicate, that also suberized roots have a significant influence on rhizosphere soil solution chemistry. This revised version was published online in June 2006 with corrections to the Cover Date.     

Spatial and temporal variation of soil solution chemistry and ion fluxes through the soil in a mature Norway Spruce (Picea abies (L.) Karst.) stand

In this study we investigated the spatial and temporal variation in soil solution chemistry and of water and ion fluxes through the soil in a forest ecosystem. Our aim was to evaluate the relevance of these variations for the accuracy of average areal soil solution concentrations and ion fluxes with seepage at 90 cm depth.Twenty spatially distinct subcompartments of approximately 1 m² were established within a mature stand of Norway spruce and ceramic suction lysimeters were installed at depths of 20, 35 and 90 cm. A tensiometer was placed close to each suction lysimeter, and one throughfall sampler was established for each subcompartment.Soil solution samples were analysed for major ions (H⁺, Na⁺, K⁺, Ca²⁺, Mg²⁺, Mn²⁺, Fe³⁺, Al³⁺, Cl^-, NO ₃ ^- , SO ₄ ^2- . We calculated water fluxes for each subcompartment separately by a numeric simulation of the soil water flux close to the lysimeters. The ion fluxes at each lysimeter were calculated by multiplying the simulated water fluxes with the ion concentrations on a fortnightly base. Averaging these 20 independent ion fluxes gave the areal average flux and an estimate of its statistical accuracy. The spatial variation of ion concentrations in the soil solution was high with coefficients of variance ranging from 5% to 128%. Part of the spatial variation was related to stem distance. Temporal variation of the concentrations was less than spatial for most ions. The spatial variation of water and ion fluxes with seepage was also substantial; for example the fluxes of SO ₄ ^2- -S calculated for each subcompartment ranged from 21 to 119 kg ha^-1 yr^-1, with an arithmetic average of 47 kg ha^-1 yr^-1. For H₂O, Mg²⁺, Cl^-, and SO ₄ ^2- , the spatial heterogeneity of seepage fluxes was largely explained by the heterogeneity of throughfall fluxes. No such relationship was found for nitrogen.Despite using 20 replicates, the 95% confidence intervals of the average annual areal fluxes with seepage were found to be 20–30% for most ions.     

Microscale heterogeneity of acidity related stress-parameters in the soil solution of a forested cambic podzol

Acid related stress in soils might be caused by high concentrations of H⁺ and Al³⁺ in soil solution. Sampling of soil solution so far integrates over a relatively large soil volume, in the range of dm³. In order to study the microscale heterogeneity of acidity related stress-parameters the soil profile of a podzolic cambisol was covered by a 10×6 matrix of micro suction cups with a grid distance of 2 cm. The soil solution collected at 10 sampling events was analyzed for free cations and anions by capillary electrophoresis and for total metal content by a micro injection technique on ICP-OES. pH and UV absorption were also measured.There was a general trend of increasing pH and decreasing UV absorption with increasing soil depth, however without a clear correlation of concentration isolines to soil horizon borders. The latter was also true for total Al (Al_tot) and Al³⁺, with the exception of the soil horizon border A_he/B_h,which was very well reflected by Al³⁺ and also by the fraction of bound Al. In the A_he horizon less than 30%, in deeper mineral soil less than 50% of Al_tot were present as free Al³⁺. This fact is critical when calculating Ca/Al ratios as a stress parameter, because total metal content measured by ICP clearly overestimates the risk of root damage, even in deeper horizons of acid forest soils, where organic complexation of Al is of minor importance. The heterogeneity of soil solution chemistry and toxicity parameters on the cm-scale was found to be significant, for example with gradients of more than 0,5 pH-units within 2 cm. Because plant roots also experience soil on a microscale, high resolution investigations of soil solution chemistry offer a new approach for looking at the chemical environment relevant for root growth and plant nutrition.     

Temporal variability of solution Cd2+ concentration in metal-contaminated soils as affected by soil temperature: consequences on lettuce (Lactuca sativa L.) exposure

The aim of this study was to assess how the solubility and the speciation of Cd in soil solution were affected over time by the soil temperature for three metal-contaminated soils. The changes of solution Cd concentration (either total or free ionic) and other physico-chemical parameters (e.g. pH, ionic strength, the concentrations of ${\text{NO}}_3^ - $ , ${\text{SO}}_4^{2 - } $ , Ca, Mg and dissolved organic carbon) were monitored over a 28-day culture of lettuce (Lactuca sativa L.) in soils incubated at 10°C, 20°C or 30°C. The major result of this study was that Cd²⁺ concentration greatly varied over time in soil solution. The Cd²⁺ concentration declined over time in soil solution as did the concentration of cations that may compete for adsorption (Ca²⁺, Mg²⁺). The rise in soil temperature primarily impacted on the concentration of Cd²⁺ via promoting the microbial C-degradation and, thus, the complexation of Cd in soil solution. The integration of the temporal variations in Cd²⁺ concentration through the calculation of the root exposure to solution Cd (E _Cd) provided a fairly close and robust prediction of Cd concentration in lettuce roots. The present work thus provided new insights on the fate of Cd in contaminated soils that may be relevant for predicting the root uptake of Cd.     

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.     

The Influence of Phytophthora citricola on Rhizosphere Soil Solution Chemistry and the Nutritional Status of European Beech Seedlings

In a rhizotron experiment the influence of Phytophthora citricola on root development, rhizosphere chemistry and nutritional status of beech seedlings was studied. After infection, the fine root system was seriously damaged and 6 weeks after inoculation some seedlings died. Plants infected with Phytophthora citricola had less steep concentration gradients of K⁺, Ca²⁺, Mg²⁺ and NO in the rhizosphere soil solution as compared with uninfected seedlings, which indicates reduced activity in nutrient uptake. It is concluded that plants try to compensate their deficit in fine root biomass and nutrient acquisition by retranslocation of nutrients.     

Plant induced alteration in the rhizosphere and the utilisation of soil heterogeneity

Plant-soil interactions result in a special rhizosphere soil chemistry, differing from that of the bulk soil found only a few mm from the root. The aim of this study was to investigate adaptation mechanisms of herbs growing in acid soils through studying their rhizosphere chemistry in a greenhouse experiment and in a field study. Ten herbs were grown in acid soil (pH 4.2 in the soil solution) in the greenhouse. The concentrations of NO₃ ^-, SO₄ ^2-, phosphates, Ca²⁺, Mg²⁺, Mn²⁺, K⁺, Na⁺, NH₄ ⁺ and pH were analysed in soil solutions obtained by centrifugation. The general pattern found was a depletion of nutrients in the rhizosphere compared with their concentrations in the bulk soil. The pH increase (up to 0.7 units) in the rhizosphere soil appeared to be caused by plant uptake of NO₃ ^- (r²=0.88). The ion concentrations in the soil solution of the rhizosphere were dependent on plant species and biomass increase. Although species with a larger biomass and higher growth rates showed a higher degree of ion depletion (except for Na⁺, SO₄ ^2-) in the rhizosphere, there were also species specific responses. A field study of five herbs at five oak forest sites in Southern Sweden (Scania) was also carried out. In addition to the soil solution concentrations, the loss on ignition (LOI) and the concentrations of 0.1 M BaCl₂ extractable K⁺, Mg²⁺, Mn²⁺, Ca²⁺, and Al ions were measured. The amount of soil solution Al was determined as free ionic (quickly reacting) Al. For all species and sites, the LOI and the concentrations of exchangeable cations were higher in the rhizosphere than in the bulk soil, apparently due to the roots preferably growing at organic-rich microsites. The concentrations of the ions as measured in the centrifuged soil solution, were either higher in the rhizosphere than in the bulk soil or were the same in both, except for NO₃ ^- and quickly reacting Al. The lower concentrations of quickly reacting Al in the rhizosphere, compared with the bulk soil could indicate the uptake of Al by the plant or the exudation of complexing substances. The pH differences were only small and mostly non-significant. Plant-soil interactions and the ability of plants to utilise heterogeneity of the soil appear to be more important for plant growth in acid soils than recognised heretofore. Rhizosphere studies provide an important means of understanding plant strategies in acid soils. This revised version was published online in June 2006 with corrections to the Cover Date.     

Illite transformation and potassium release upon changes in composition of the rhizophere soil solution

Aims and background

Release of ‘non-exchangeable’ potassium (K) from interlayers of illite is diffusion-controlled and has been shown to depend on the solution concentration of K and other cations (Ca²⁺, Mg²⁺, NH₄ ⁺).

Methods

We analysed changes in soil solution concentrations of K and competing cations in situ at different distances from the root surface over time and related them to the transformation of illite, as revealed by X-ray diffraction, and chemical measures of differently bound K.

Results and Conclusions

Within 49 and 98 days, respectively, 6.4 and 14.4 % of the illite’s total K was released upon contact with the root system. Mixed layered minerals increased from 33 (0 d) to 35 (49 d) to 40 % (98 d). Release of K from interlayers and the transformation of illite occurred at soil solution K concentrations close to the threshold of 80 μM suggested earlier. Concentrations of Ca and Mg increased with decreasing distance from the root surface, promoting the release of K. The NaBPh₄ method supposed to determine ‘non-exchangeable’ K extracted only 1/3 of the total K from illite.     

Role of calcium and other ions in directing root hair tip growth in Limnobium stoloniferum

The magnitude and spatial localization of Ca²⁺, K⁺ and H⁺ fluxes in growing and non-growing Limnobium stoloniferum root hairs was determined using non-invasive, ion-selective vibrating microelectrodes. Both the spatial pattern and magnitude of the ionic flux was dependent on the particular ion in question. Both H⁺ and Ca²⁺ influx was localized almost exclusively to the tips of growing root hairs, suggesting that these fluxes may be involved in directing growth. Influx of K⁺ showed no distinct localization and uptake appeared uniform along the length of the root hair. Competitive inhibition of Ca²⁺ influx using a range of Mg⁺ concentrations indicated that the magnitude of the Ca²⁺ flux entering the root hair tip did not determine growth rate; however, the presence of Ca²⁺ on the external face of the membrane was implicit for root hair integrity. Aluminum proved to be a potent inhibitor of root hair growth. At an exogenous Al concentration of 20 M a complete blockage of Ca²⁺ influx into root hair tips was observed, suggesting that Al blockage of Ca²⁺ influx could be involved in Al toxicity. However, at a lower Al concentration (2 M), Ca²⁺ fluxes were unaffected while inhibition of growth was still observed along with a distinct swelling of the root hair tip. The swelling at the root hair tips was identical in appearance to that seen in the presence of microtubule inhibitors, suggesting that Al could influence a number of different sites at the plasma-membrane surface and within the cell. The possible role(s) of Ca²⁺ and H⁺ fluxes in directing tip growth are discussed.     

Nutrient concentration in wheat and soil under allelopathy treatments

Allelopathy is related to soil nutrient availability and allelochemicals can change the soil and therefore the plant nutrient status. Wheat is one of the most important crops for the production of human food in the world. Alhagi maurorum and Cardaria draba are the most important weeds in wheat fields. We performed experiments to assess the allelopathic effect of A. maurorum and C. draba shoots on mineral nutrient concentrations in pot-grown wheat plants and soil. The presence of dry powder of A. maurorum and C. draba shoots reduced concentrations of macronutrients (NO₃ ^?, K⁺, Ca²⁺ and P) and micronutrients (Fe²⁺ and Cu²⁺) in roots and shoots of wheat plants, whereas it did not affect concentrations of Mg²⁺, Mn²⁺ and Zn²⁺. Allelopathic effect of A. maurorum was significantly greater than that of C. draba. There was a significantly positive correlation between wheat growth and ion concentration. There was a significantly negative correlation between the soil nutrient concentration and plant nutrient concentration across the treatments. These results suggest that allelopathy increases the nutrient availability in the soil because of the decrease in absorption by plants.     

凋落物和根系输入对南亚热带季风常绿阔叶林土壤养分的影响

植被凋落物和根系输入在调节森林土壤元素生物地球化学循环中扮演着关键作用。目前仍然不清楚凋落物和根系输入对热带原始林土壤主要元素含量的调控作用。针对该研究现状,以中国南亚热带季风常绿阔叶林为研究对象,通过开展凋落物与根系输入改变的控制试验（6个处理,每处理4次重复：对照、凋落物加倍、凋落物去除、断根、断根+凋落物加倍、断根+去除凋落物）,探讨了凋落物和断根处理对土壤可溶性离子、土壤酸中和能力（ANC）和阳离子交换量（CEC）的短期影响。凋落物与根系处理半年后的结果显示：（1）凋落物去除与加倍处理都显著增加了0-40 cm土壤NO₃^-含量,并且凋落物去除效应大于添加效应;去除凋落物增加了表层土壤（0-20 cm） Ca²⁺、Mg²⁺、Na⁺的含量。（2）断根处理显著增加0-40 cm土壤NO₃^-和表层土壤Ca²⁺、Mg²⁺含量。（3）断根和去除凋落物交互处理显著增加了0-40 cm土壤NO₃^-和表层土壤Ca²⁺、Mg²⁺、K⁺含量,产生了叠加效应。（4）凋落物和断根处理并没有改变土壤pH,但降低了土壤酸中和能力（除凋落物加倍外）,其降低的原因主要与阳离子交换量的降低和NO₃^-含量的增加有关。这些结果表明,土壤养分离子的可利用性（尤其是NO₃^-和Ca²⁺、Mg²⁺）和酸缓冲能力对凋落物和根系输入改变响应敏感,森林植物及其凋落物对土壤养分保留和缓冲性能具有重要调节作用。在人为干扰和气候变化加剧背景下,该研究可为森林生态系统可持续管理提供重要的理论参考。此外,植被凋落物和根系输入改变引起的长期生态学效应仍值得进一步关注。     

Diel plant water use and competitive soil cation exchange interact to enhance NH<Subscript>4</Subscript><Superscript>+</Superscript> and K<Superscript>+</Superscript> availability in the rhizosphere

Aims

Hydro-biogeochemical processes in the rhizosphere regulate nutrient and water availability, and thus ecosystem productivity. We hypothesized that two such processes often neglected in rhizosphere models — diel plant water use and competitive cation exchange — could interact to enhance availability of K⁺ and NH₄ ⁺, both high-demand nutrients.

Methods

A rhizosphere model with competitive cation exchange was used to investigate how diel plant water use (i.e., daytime transpiration coupled with no nighttime water use, with nighttime root water release, and with nighttime transpiration) affects competitive ion interactions and availability of K⁺ and NH₄ ⁺.

Results

Competitive cation exchange enabled low-demand cations that accumulate against roots (Ca²⁺, Mg²⁺, Na⁺) to desorb NH₄ ⁺ and K⁺ from soil, generating non-monotonic dissolved concentration profiles (i.e. ‘hotspots’ 0.1–1 cm from the root). Cation accumulation and competitive desorption increased with net root water uptake. Daytime transpiration rate controlled diel variation in NH₄ ⁺ and K⁺ aqueous mass, nighttime water use controlled spatial locations of ‘hotspots’, and day-to-night differences in water use controlled diel differences in ‘hotspot’ concentrations.

Conclusions

Diel plant water use and competitive cation exchange enhanced NH₄ ⁺ and K⁺ availability and influenced rhizosphere concentration dynamics. Demonstrated responses have implications for understanding rhizosphere nutrient cycling and plant nutrient uptake.

     

Cortical cell fluxes and transport to the stele in excised root segments of Allium cepa L.

Summary From compartmental analysis of radioisotope elution measurements, concentrations and fluxes of Mg²⁺ were estimated for cortical cells in root segments of onion, Allium cepa L., relative to a complete nutrient solution containing 0.25 mM Mg²⁺. Five compartments for Mg²⁺ in the cortex were found and, in order of increasing rates of exchange, identified with the vacuoles and the cytoplasm of the cortical parenchyma, the Donnan free space, the water free space, and the superficial film of solution on the segments. With the Ussing-Teorell flux ratio equation as the criterion, it was concluded that Mg²⁺ entered the cytoplasm passively and was actively pumped back across the plasmalemma. Mg²⁺ concentration in the vacuole could be estimated only as lying between wide limits (1.3 to 14.3 eq ml^-1), but whatever the concentration within this range, it was concluded that Mg²⁺ was passively distributed across the tonoplast. Net flux was zero and the vacuolar concentration commensurate with this was found to be 6.6 eq ml^-1. The transported fraction of total efflux, appearing at the segment cut ends, was estimated separately. Magnesium was found to be transported almost exclusively in the basipetal direction.     

Occurrence and intensity of wild boar disturbances, effects on the physical and chemical soil properties of alpine grasslands

Background and aims

Physical and chemical soil properties determine local plant conditions and resources, affecting plants’ ability to respond to disturbances. In alpine grasslands, wild boar disturbances occur at different intensities, what may affect differently their soil properties. Alpine soils from five contrasted plant communities were explored within and outside disturbances, accounting for an overall and community scale effect. Additionally, we analysed the effect of disturbance intensity on soil NO₃ ^--N and NH₄ ⁺-N.

Methods

Soils were analyzed for physical (bulk density, moisture content and electrical conductivity), and chemical properties (pH, total N and C, oxidizable C, C:N ratio, available K, P, Ca²⁺, Na⁺ and Mg²⁺). Resin bags were used to compare the effect of the disturbance occurrence and intensity on soil NO₃ ^--N and NH₄ ⁺-N.

Results

Bulk density, total N and NO₃ ^--N concentration were significantly higher in disturbed areas, while soil moisture, C:N, NH₄ ⁺-N, Na⁺, Mg²⁺ and Ca²⁺ concentrations were significantly lower. However, low disturbance intensity reduced NO₃ ^--N and increased NH₄ ⁺-N concentrations.

Conclusions

Wild boar occurrence and intensity strongly alter physical and chemical conditions of alpine soils, increasing soil compaction, and altering the availability of N forms. These changes may affect most plant species, thus affecting the structure and dynamics of alpine plant communities.     

盐渍土壤大果沙枣树主要矿质阳离子的吸收和分配特征

为探明大果沙枣树体矿质离子渗透调节机制,比较分析了盐渍化生境中1～12a生树的根、枝和叶部主要矿质阳离子的吸收、分配特征。结果表明:(1)大果沙枣树体内Ca~(2+)的积累量最高(13.79 g/kg),K~+次之(5.92 g/kg),Na~+最低(1.00 g/kg);随着树龄的增大,大果沙枣根部的Na~+以及枝和叶部的K~+、Ca~(2+)、Mg~(2+)的积累量均逐渐增大,而根部的K~+含量则逐渐减少;高龄段(10～12a)树体根部的Na~+累积量显著(P0.05)高于中低龄(1～9a)段。(2)大果沙枣树体内K~+/Na~+最大(15.36),Mg~(2+)/Na~+次之(12.25),Ca~(2+)/Na~+最小(10.51),根和枝部的K~+/Na~+均随着树龄的增大而降低,叶部则表现相反。(3)土壤中的K~+和Mg~(2+)向根方向、根部K~+、Mg~(2+)和Ca~(2+)向枝方向以及根部的K~+和Mg~(2+)向叶方向的选择运移系数均随着树龄的增大呈直线上升趋势。(4)土壤中Na~+与根部Na~+含量呈极显著正相关关系(0.687,P0.01),与叶部的K~+含量呈显著正相关(0.605,P0.05);土壤中K~+含量与根部的Na~+、叶部的K~+分别呈显著和极显著正相关(0.544,0.676),与根部的Mg~(2+)呈显著负相关关系(-0.499)。研究发现,大果沙枣树生长过程中主要通过根部对Na~+的聚积作用,以及K~+、Mg~(2+)和Ca~(2+)在枝、叶部的吸收积累来维持植物体离子平衡,以适应盐渍土壤环境。     

Acidification of freshwaters by red soil in a subtropical silicate rock area,Okinawa, Japan

Two samples of red soil, one from Gushikawa Recreation Center (GRC) and one from Okinawa Royal Golf Club (ORGC), were examined for particle size distribution, textures, minerals, and chemical compositions. The effects of particle size and grinding of clay minerals on pH, electrical conductivity (EC), and dissolved chemical species were studied in deionized water and river water. The results of red soil solutions were compared with those of acidic waters found in red soil dominated areas. The minimum pH values of soil solutions extracted by deionized water were 4.38–5.36 and 5.16–5.89 and the maximum values of EC were 4.91–16.98mSm^–1 and 3.54–11.23mSm^–1 for GRC and ORGC, respectively. In the river water samples equilibrated with red soils, the minimum pH values were 4.48–5.10 and 4.77–5.91 and the maximum EC values were 19.6–34.2mSm^–1 and 17.5–25.0mSm^–1 for GRC and ORGC, respectively. The values of pH and EC varied with the soil–solution ratio and the particle size. The chemical composition of river water without mixing with red soil shows Na⁺K⁺ and Ca²⁺Mg²⁺. After mixing with red soil, the trend of the concentrations changed to Na⁺K⁺ and Mg²⁺Ca²⁺, which is the same as that of soil solutions in deionized water as well as that of acidic waters found in the red soil area. The pH of the acidic waters was 4.95–5.81 and EC was 7.76–30.0mSm^–1. Laboratory experimental results agreed well with those found in the field in terms of trend of concentrations of the chemical species and pH. Therefore, the results of this study suggest that the low pH and trend of the concentrations of chemical species of the acidic waters found in the red soil dominated areas were the result of the interaction of natural water and red soil.     

Reversibility of damages to forest floor plants by episodes of elevated hydrogen- and aluminium-ion concentrations in the soil solution

Herbs and grasses may episodically be exposed to elevated concentrations of potentially toxic elements as H⁺ and Al³⁺ due to considerable temporal variability in the chemical composition of soil solutions in the uppermost layer of the soil profile. Greenhouse experiments were performed to test the effect of episodes of different length (1 and 2 weeks) and concentrations of H⁺ and Al³⁺ (pH 3.8, 4.0, 4.2 and 4.5; 0, 20 and 70 M Al) on root and shoot growth, designed to elucidiate the reversibility of growth inhibition. Three forest floor species were studied-Galium odoratum and Lamium galeobdolon, having similar pH distribution ranges in the field and Poa nemoralis which also occurs at slightly lower pH. The plants were grown for 5 weeks (episode and recovering time) in a synthetic soil solution in a flowing solution system without recirculation. The species reacted in three different ways. Galium odoratum was the most sensitive species and seemed to be irreversibly damaged (ceased growth) by 2 week episodes of pH4.0 and Al20 M at pH4.2. Lamium galeobdolon was about equally sensitive during the episodes but it had a much greater ability to recover. Poa nemoralis was rather insensitive to the episode treatments tested. It is concluded that episodes of elevated H⁺ and Al³⁺ concentrations may be decisive for plant performance. It is therefore important to consider the extreme environmental conditions which plants may be exposed to in the field, in addition to long-term averages of e.g. soil solution concentration of potentially toxic elements, when studying species distribution and performance in relation to soil chemical properties.     

Effects of air pollutant-temperature interactions on mineral-N dynamics and cation leaching in reciplicate forest soil transplantation experiments

Increased emissions of nitrogen compounds have led to atmosphericdeposition to forest soils exceeding critical loads of N overlarge parts of Europe. To determine whether the chemistry offorest soils responds to changes in throughfall chemistry, intactsoil columns were reciprocally transplanted between sites, withdifferent physical conditions, across a gradient of N and Sdeposition in Europe.The transfer of a single soil to the various sites affected itsnet nitrification. This was not simply due to the nitrificationof different levels of N deposition but was explained bydifferences in physical climates which influenced mineralizationrates. Variation in the amount of net nitrification between soiltypes at a specific site were explained largely by soil pH.Within a site all soil types showed similar trends in netnitrification over time. Seasonal changes in net nitrificationcorresponds to oscillations in temperature but variable time lagshad to be introduced to explain the relationships. WithArrhenius law it was possible to approximate gross nitrificationas a function of temperature. Gross nitrification equalled netnitrification after adaptation of the microbial community oftransplanted soils to the new conditions. Time lags, andunderestimates of gross nitrification in autumn, were assumed tobe the result of increased NH ₄ ⁺ availability due either tochanges in the relative rates of gross and net N transformationsor to altered soil fauna-microbial interactions combined withimproved moisture conditions.Losses of NO ₃ ^- were associated with Ca²⁺and Mg²⁺ in non-acidified soil types and with losses ofAl³⁺ in the acidified soils. For single soils the ionequilibrium equation of Gaines-Thomas provided a useful approximationof Al³⁺ concentrations in the soil solution as a functionof the concentration of Ca²⁺. The between site deviationsfrom this predicted equilibrium, which existed for single soils, couldbe explained by differences in throughfall chemistry which affectedthe total ionic strength of the soil solution.The approach of reciprocally transferring soil columnshighlighted the importance of throughfall chemistry, interactingwith the effect of changes in physical climate on forest soilacidification through internal proton production, in determiningsoil solution chemistry. A framework outlining the etiology offorest die-back induced by nitrogen saturation is proposed.     

增温和施氮对亚热带杉木人工林土壤溶液养分的影响

在增温和氮沉降等气候变化背景下,土壤溶液养分元素供应是否平衡对加速或减弱土壤养分循环起着至关重要的作用。为探究增温和施氮对亚热带杉木人工土壤溶液养分动态的影响,分别于各样地的0—15、15—30cm和30—60cm土层安装土壤溶液采集器。利用真空泵的负压原理采集土壤溶液,对其有机组分及无机组分进行了两年的动态监测。结果显示:增温及增温+施氮显著增加了各土层溶解性总氮(DTN)及硝态氮(NO-3)浓度,而施氮促进了植被对其的大量吸收而未呈现显著的促进作用。整体而言,短期增温和施氮处理显著降低了可溶性有机碳(DOC)浓度,对土壤溶液K~+、Ca~(2+)、Na~+、Mg~(2+)等离子含量影响较小。但相比于施氮,增温对土壤溶液中矿质元素的影响远大于施氮。增温导致的土壤孔径增大,通透性增强可极大地促进Fe~(3+)、Al~(3+)淋溶,同时导致表层Na~+、Mg~(2+)离子含量显著降低。增温+施氮交互作用对土壤溶液各养分的影响存在叠加效应,但并不是增温和施氮单因子的简单累加,要深入了解土壤养分对未来气候变迁的内部机制需进一步长期监测。