Decomposition of litter from three major plant species of jarrah (Eucalyptus marginata Donn ex Sm.) forest in relation to site fire history and soil type

Rates of weight loss and release of N, P, K, S, Ca, Mg, Na, and Cl from litter of several species in jarrah (E. marginata Donn ex Sm.) forest were measured in relation to site fire history and soil type. Weight loss from leaf litter decreased in the order jarrah > marri (E. calophylla R. Br. ex Lindl.) > Banksia grandis Willd. After 18 months on the forest floor senesced leaves of jarrah, marri and Banksia had lost 45%, 42% and 19%, respectively, of their original weight. Although greatest rates of decomposition occurred on a site burnt 3 y previously by an intense autumn fire and slowest rates on a site which had not been burnt for 8 y, the differences between burn sites were small in comparison with the total weight loss from decomposing litter. The order of release of nutrients from decomposing eucalypt litter was P<N<Ca<S<Mg<Cl<K<Na. There appears to be only slow release of N and P from the litter layer of these forests in the period between successive control burns. Fresh jarrah leaves, which are similar in chemical composition to leaf litter falling after crowns have been scorched by intense fire, decompose rapidly in comparison with senescent leaf tissue. Release of nutrients, particularly N and P, is also more rapid from fresh leaves than from leaf litter. Rates of decomposition of green leaves differed between soil types in the order reddish gravels > dark sandy duplex soil > yellow gravels. These differences may be related to the higher nutrient status of the reddish gravel soils.     

Brachythecium complexum J.D.Orgaz,sp. nov., a new species from Japan

Abstract

Two types of fires were distinguished, rapid fires and bonfires, the amount of ash deposited and the intensity of heating both being greater during a bonfire. Rapid-fire sites are recolonized largely by the pre-burn species, but on bonfire sites, after an initial delay period, in which both angiosperm and bryophyte growth is inhibited, a characteristic bonfire community is formed in which Funaria hygrometrica is the most conspicuous species. Field experiments and soil analyses confirmed that edaphic conditions were of primary importance in determining the establishment of the bonfire community and showed that a major difference between the two sorts of fire lay in their effect on the surface soil.

After a bonfire, high concentrations of soluble organic matter and inorganic nutrients were found. With the exception of the calcium concentrations, these decreased with time, the levels of potassium, magnesium and phosphorus approaching or even reaching those of the unburnt soil after 18 months. It seems very likely that after an initial increase in the levels of both ammonium- and nitrate-nitrogen, the rate of nitrification would be stimulated and remain high for a considerable length of time. Rapid fires, as expected, appeared to have relatively little effect on the surface soil, levels of calcium and phosphorus in particular were never as high as in bonfire soils and it is most unlikely that there was any stimulation of nitrification.     

Wood-ash recycling affects forest soil and tree fine-root chemistry and reverses soil acidification

Wood ash was applied to a forest ecosystem with the aim to recycle nutrients taken from the forest and to mitigate the negative effects of intensive harvesting. After two years, the application of 8,000 kg ha⁻¹ of wood ash increased soil exchangeable Ca and Mg. Similarly, an increase in Ca and Mg in the Norway spruce fine roots was recorded, leading to significant linear correlations between soil and root Ca and soil and root Mg. In contrast to these macronutrients, the micronutrients Fe and Zn and the toxic element Al decreased in the soil exchangeable fraction with the addition of wood ash, but not in the fine roots. Only Mn decreased in soil and in fine roots leading to a significant linear correlation between soil and root Mn. In soil, as well as in fine roots, strong positive correlations were found between the elements Ca and Mg and between Fe and Al. This indicates that the uptake of Mg resembles that of Ca and that of Al that of Fe. With the wood ash application, the pH increased from 3.2 to 4.8, the base saturation from 30% to 86%, the molar basic cations/Al ratio (BC/Al) of the soil solution from 1.5 to 5.5, and the molar Ca/Al ratio of the fine roots from 1.3 to 3.7. Overall, all below-ground indicators of soil acidification responded positively to the wood ash application within two years. Nitrate concentrations increased only slightly in the soil solution at a soil depth of 75–80 cm, and no signs of increased heavy metal concentrations in the soils or in the fine roots were apparent. This suggests that the recycling of wood ash could be an integral part of sustainable forest management because it closes the nutrient cycle and reverses soil acidification.     

Abrupt increase in phosphorus and potassium fluxes during a masting event in a Bornean tropical forest

Mechanisms by which the productivity of tropical ecosystems is limited by nutrients is a long-standing question, but little information is available on the nutrient dynamics supporting the masting phenomenon in Southeast Asian evergreen rainforests. In this study we examined the nutrient sink and potential nutrient sources of masting in a Bornean tropical forest. We investigated if nutrient flux in fine litter, tree stems, and soils changed temporally in response to intense flower and fruit production. Fifty-five litter traps were installed in a 2-ha plot at the onset of flowering (April 2010), and litter and nutrient fluxes were monitored for more than 4 years (May 2010–December 2014). Wood cores of trunks and coarse roots of abundant species (Shorea spp.) and soil samples were collected in May 2010, September 2010, and September 2011 (coinciding with peak flowering, peak fruiting, and 1 year after fruiting, respectively). The P and K fluxes in the total litter were significantly greater in the mast year (2010) than non-mast years, whereas the Mg, N, and Ca fluxes did not vary in relation to masting. In line with the nutrient fluxes, P and K concentrations in coarse roots of flowering individuals of S. multiflora decreased in September 2011. The present results suggest that tropical trees require extraordinary amounts of P and K for masting, and may retranslocate stored nutrients to meet the elevated nutrient demands for masting.     

Establishment of microscale vegetation pattern in maritime chaparral after fire

We quantified microscale pattern in vegetation and seed assemblages along a 24 m transect before and for two years following a controlled burn in chamise (Adenostoma fasciculatum) chaparral in central coastal California. Our objective was to document scale-dependent correlation between pre-burn seed assemblages, pre-burn canopy cover, microtopography, soil temperatures during burning, post-burn seed assemblages and post-burn vegetation. Scale-dependent correlations among pre- and post-burn seed densities, maximum soil temperatures during burning, microtopography and post-burn vegetation were measured based on two-term local covariance analysis.Seed distribution varied among species prior to fire, with seeds of some annual species concentrated in gap areas. Maximum soil temperatures during burning ranged from less than 50 °C to 225 °C, and were generally lowest in gaps in the pre-burn canopy. These gaps were associated with local topographic depressions. After burning, readily germinable seeds were concentrated in or near gaps in the pre-burn canopy. Germination of different species was variously enhanced, diminished or unchanged by the passage of fire. Post-burn vegetation was very patchy, with some areas nearly devoid of seedlings and other areas, especially pre-burn canopy gaps, supporting numerous seedlings. Seedling recruitment patterns in the second year were generally highly correlated with patterns in pre-burn seed banks and first year vegetation. Although many species exhibited similar recruitment patterns, several different mechanisms may have been responsible for the origin of those patterns.     

Effect of wood ash application on soil solution chemistry of tropical acid soils: incubation study

The objective of this study was to determine the effect of wood ash application on soil solution composition of three tropical acid soils. Calcium carbonate was used as a reference amendment. Amended soils and control were incubated for 60 days. To assess soluble nutrients, saturation extracts were analysed at 15 days intervals. Wood ash application affects the soil solution chemistry in two ways, as a liming agent and as a supplier of nutrients. As a liming agent, wood ash application induced increases in soil solution pH, Ca, Mg, inorganic C, SO4 and DOC. As a supplier of elements, the increase in the soil solution pH was partly due to ligand exchange between wood ash SO4 and OH- ions. Large increases in concentrations of inorganic C, SO4, Ca and Mg with wood ash relative to lime and especially increases in K reflected the supply of these elements by wood ash. Wood ash application could represent increased availability of nutrients for the plant. However, large concentrations of basic cations, SO4 and NO3 obtained with higher application rates could be a concern because of potential solute transport to surface waters and groundwater. Wood ash must be applied at reasonable rates to avoid any risk for the environment.     

种植Bt玉米及秸秆还田后土壤中Bt蛋白的变化及其对土壤养分的影响

在大棚水泥池内种植两个Bt玉米(5422Bt1和5422CBCL)及其同源常规玉米5422,研究了种植Bt玉米及秸秆还田过程中根际土、根围土、3层根外土(0～20、20～40和40～60 cm)中Bt蛋白含量的时空动态特征及其对土壤养分含量的影响．结果表明： 种植Bt玉米和常规玉米后,根围土(种植后90 d)和3层根外土(种植后30、60和90 d)中均检测到少量的Bt蛋白(含量<0.5 ng·g^-1),在Bt玉米5422Bt1和5422CBCL根际土中则分别检测到1.59和2.78 ng·g^-1的Bt蛋白．玉米秸秆还田后,Bt蛋白能在3 d内快速降解,在还田后第7天只检测到少量的Bt蛋白．与常规玉米5422相比,种植Bt玉米5422Bt1 90 d后根围土和3层根外土中有机质、速效养分(碱解氮、速效磷和速效钾)和全量养分(全氮、全磷和全钾)含量均没有显著差异;5422Bt1秸秆还田60 d后0～20 cm土层的有机质和全氮含量显著升高,速效钾含量显著降低,而其他养分指标则没有显著差异,20～40 cm和40～60 cm土层的所有养分指标均没有明显差异．种植Bt玉米5422CBCL后根围土中仅速效磷含量显著低于种植常规玉米5422,但0～20 cm土层中全磷含量显著提高,其他养分指标均没有差异;还田5422CBCL秸秆后仅0～20 cm土层的速效磷含量显著高于常规玉米5422．研究结果表明,通过玉米根系分泌和秸秆分解进入土壤的Bt蛋白不会在土壤中累积,对养分含量也基本没有显著影响.
     

The effects of burning on the understorey composition of 11–13 year-old rehabilitated bauxite mines in Western Australia – Vegetation characteristics

Alcoa of Australia Limited has been rehabilitating bauxite mines in the jarrah (Eucalyptus marginata) forest of Western Australia for more than 30 years. Mines rehabilitated in the early 1980s using out-dated methods have built up substantial fuel loads that may be reduced through prescribed burning. The vegetation response of 11–13 year-old rehabilitated bauxite mines to fire regimes differing in intensity and season over the first two years of post-burn succession is compared to the native jarrah forest. A total of 243 species from 137 genera and 56 families were identified in the native forest reference sites and in the 11–13 year-old rehabilitated areas before and after burning. The vegetation of the pre-burn rehabilitated areas was very different to that of the native jarrah forest. While total live plant cover, Acacia density, non-native eucalypt seedling density, weed density and the evenness index were similar between the two areas, total plant density, live Acacia cover, the proportion of weeds, native species numbers and diversity were significantly different. However, the greatest difference between the vegetation of the pre-burn rehabilitated sites and the native jarrah forest was the higher dominance of seeding species (plants killed by fire) in rehabilitated areas. In contrast, native jarrah forest was dominated by resprouting species (plants that survive fire). Burning the rehabilitated sites was successful in making the areas more similar to the forest in terms of total plant density, live Acacia cover and native species numbers but decreased their similarity in terms of live plant cover, Acacia density, non-native eucalypt seedling density, weed density and evenness. The vegetation response of the rehabilitated areas to different seasons of burning showed that autumn burning led to a greater increase in plant establishment than spring burning. Autumn burning also resulted in an undesirable increase in the density of non-native eucalypt seedlings that was not observed following spring burning. Although burning these 11–13 year-old rehabilitated sites will increase similarity to the native forest, it is unlikely that they will resemble the native jarrah forest without further management intervention.     

Frequent fire affects soil nitrogen and carbon in an African savanna by changing woody cover

When tropical and sub-tropical ecosystems burn, considerable amounts of N present in the biomass fuel may be released. This ultimately results in a loss of fixed N to the atmosphere. It is often assumed that this volatilization loss of N with frequent fire will result in a reduction of plant-available N and total system N. By changing the amount of woody biomass fire may, however, also have indirect effects on N and C dynamics. Here we consider the effects of 50 years of frequent fire on total soil N and soil organic C (SOC) and total soil N in a mesic savanna in the Kruger National Park, South Africa. We also determine how changes in woody biomass may affect total soil N and SOC. We measured soil and fine root N and C concentrations as well as total soil N and SOC pools in four burning treatments, including fire exclusion, of a long-term fire experiment. Our results show that regardless of soil depth, fire treatment had no significant effect on total soil N and SOC. Our results also show that under trees total soil N and SOC concentrations of the surface soil increase, and pools of N and SOC increase to a depth of 7 cm. However, the extent to which soil N and C dynamics differed under canopies and away from canopies was dependent on fire treatment. Our results show that the effect of fire on soil N and C is mediated both through the indirect effect of changes in woody cover and the direct effects of fire (volatilization losses of nutrients). We suggest that woody thickening in this mesic savanna will have pronounced effects on long-term N and C dynamics.     

亚热带典型林分对表层和深层土壤可溶性有机碳、氮的影响

林分类型是影响土壤可溶性有机碳、氮库大小的重要因素,但目前对其研究主要集中在表层土壤(0～10 cm).本研究以亚热带地区天然林、毛竹林、格式栲人工林和杉木人工林为对象,用3种不同的浸提方式(冷水、热水和KCl溶液)提取表层(0～10 cm)和深层(40～60 cm)土壤中可溶性有机碳(DOC)和有机氮(DON),研究林分类型对表层和深层土壤可溶性有机碳、氮库的影响.结果表明: 林分类型对表层土壤DOC及其占土壤总有机碳(TOC)的比重有显著影响,深层土壤受林分类型的影响不显著;不同林分土壤DON含量仅在表层土壤存在显著差异,在深层土壤差异不显著.林分间土壤微生物生物量碳的差异仅在表层土壤达到显著水平.DON占土壤总氮(TN)的比重在各林分表层和深层土壤间差异均不显著.3种浸提方法得到的DOC和DON库大小顺序为热水>KCl>冷水,不同浸提方法得到的DOC库及DON库的相关性均达到显著水平,表明冷水、热水和KCl溶液浸提得到的有机碳、氮库含有相似组分.冷水和热水浸提方法得到的表层土壤DOC和DON含量及DOC占TOC比重在天然林和毛竹林均显著大于格式栲和杉木人工林,表明天然林和毛竹林土壤可溶性有机碳、氮含量高于格式栲和杉木人工林,更有利于土壤肥力的恢复.     

Wood ash applications to temperate forest ecosystems—potential benefits and drawbacks

The objectives of the present work were (a) to quantify the effects of wood ash on forest ecosystems through a meta-analysis approach associated with a detailed review of the literature (mainly composed of work carried out in Nordic countries) and (b) to extrapolate the effects on forest growth to other contexts (i.e. warm temperate countries) by identifying the cases for which wood ash applications can be beneficial to forest production. Three databases were built regarding the effects of wood ash on soil (151 observations; 33 experimental field trials), on nutrient concentrations of tree foliage (68 observations; 28 trials) and on annual stem biomass growth rate (70 observations; 27 trials). We obtained information on the wide variability of ash properties due to differences in burnt compounds, combustion processes and ash conditioning. Two important properties of wood ash are its high pH value and neutralizing capacity. These properties result in biochemical modifications of forest soils limed with ash. In the short term, soil solution composition was dramatically modified. Intense peaks of the K, Na or SO₄ concentrations were observed, resulting from the dissolution of salts contained in ash. At the same time, Ca and Mg concentrations increased as the carbonate pool of wood ash started to dissolve. The consequence of this dissolution process was an increase in the pH in all the soil phases. These modifications increased the activity of the soil microflora and some isolated peaks in the mineralization of soil organic matter may be observed in mineral soils. In the longer term, that is to say after the first year following ash application, only the effect on the acidity status of the soil remained significant. The effects of ash addition on forest ecosystems usually increased with the dose and were more pronounced with loose ash compared to aggregated ash. The addition of wood ash into forest ecosystems increased the foliar Ca status of trees. Some modifications of other nutrients, like P or K, were also observed but only for a few years after treatment. For most stands growing on mineral soils of Nordic countries, this treatment did not result in an increase in tree growth, probably because of the absence of N in the ash. For stands growing on organic soils of the same area, this input, associated with a long-lasting increase of soil organic matter mineralization, was sufficient to improve tree growth significantly (median = +59% compared to the control). For soils located in warm temperate regions, similar responses are expected for organic soils. For mineral soils, the wood ash application is expected to be suitable for stands showing deficiencies in K, Ca or Mg. Ash may contain high amounts of toxic heavy metals such as Cd. The bioavailability of most of these elements appeared to be very low in a forest context. No contamination of food chains has been observed, except possibly via some species of fungi, and heavy metals remain in the forest litter or in the topsoil. Based on all the reviewed results, several guidelines for wood ash application into forest ecosystems are proposed. Wood ash application should be restricted to acidic soils. Applications should consist of low doses of a stabilized ash form. Wood ash should be applied to adult stands rather than onto seedlings.     

Effects of a surface wildfire on soil nutrient and microbial functional diversity in a shrubbery

The aim of the study was to determine effects of a wildfire on soil nutrients and soil microbial functional diversity in short-term time scales. Burned and unburned control soil samples were collected 1 day, and 2, 4, 8, 10, 12 and 15 months after a shrubbery fire in Yumin county of Xinjiang, Northwest China. Nutrients of soil in each sampling time were detected and soil microbial functional diversity was measured by Biolog Eco plates. Results of the study showed that soil nutrients were significantly affected by fire. Soil pH increased immediately after the wildfire and was higher than that of unburned soil during 15 months post fire. Soil organic matter and total N significantly decreased immediately after the fire and was even lower than control soil at the 15th month post fire. Soil available P level increased sharply during the 4th month after the fire, and later reached to the maximum value with eight times higher than that of unburned soil. Soil available N and available K were more than the control site in 2 months after the fire, then decreased, but available N began to increase, when vegetations restored 1 year after the fire. Soil microbial activity and functional diversity recovered gradually after fire. The average well color development (AWCD) and functional diversity indices (Shannon index, Simpson index, and McIntosh index) decreased significantly 1 day after the fire, but then increased and were similar to that of undisturbed soil 15 months after the fire, when plant started to regenerate in burned area. The changes in soil nutrients after the fire affected soil microbial activity and functional diversity. Correlation analysis revealed that AWCD was negatively correlated with soil pH and positively correlated with soil total N and available N, Shannon and Simpson index had positive significantly correlation with soil total N and McIntosh index had positive significantly correlation with available N. Result of principal component analysis based on the data of carbons metabolism showed that microbial catabolic profiles of burned soils of each sampling time after the wildfire were different and all were distinct from those of unburned soils, which might suggest that microbial community structure of fire-impacted area changed dynamically on monthly scale and was distinct from that of the control site in 15 months after fire, although microbial activity or richness showed similar to pre-fire level at the 15th month post-fire.     

Tracing water uptake by jarrah (Eucalyptus marginata) trees using natural abundances of deuterium

 Seasonal change in the δ²H content of water from twig sap, soil, rainfall and groundwater were measured to determine the water sources accessed by jarrah (Eucalyptus marginata) trees at three sites in Western Australia with differing soils and depths to water table. During winter and spring the main contributor to the water uptake of the trees was stored water in the surface layers of the soil replenished by predominantly winter rainfall. With the onset of summer drought jarrah became more reliant on water from deeper down the profile. There was no clear evidence that jarrah could tap water from groundwater more than 14 m deep in deep sands. Defining the source of water for trees in deep lateritic soils using stable isotopes is hampered by the uniform deuterium profiles down most of the unsaturated zone and into the groundwater. There was a limited response in the δ²H values of sapwater in twigs to changes in the δ²H of the upper layers of the deep sand following input of rainfall in autumn. The damped response was related to the small variation in the δ²H composition of rainfall in most events during the year and the mixing in the tree of water extracted from different locations in the soil profile. Received: 21 August 1995 / Accepted: 3 December 1995     

青海省森林细根生物量及其影响因子

细根是植物吸收水分和养分的主要器官。全球变暖背景下,研究森林细根生物量及其环境因子的变化对生态系统碳平衡、碳收支及其贡献率具有重要意义。采用土钻法和室内分析法对青海省森林6个海拔梯度上5种林分类型的细根生物量和土壤理化性质进行测定,并分析了与环境因子之间的相互关系。结果表明:(1)青海省森林0—40 cm土层总细根生物量平均为8.50 t/hm~2,随着海拔梯度的增加先降低后升高,不同海拔梯度细根生物量差异显著(P0.05),最大值出现在2100—2400 m处。(2)5种林分0—40 cm土层总细根生物量为:白桦白杨云杉圆柏山杨,不同林分间细根生物量差异不显著。(3)细根垂直分布随土层深度增加而减少,且70%的细根集中在表层(0—20 cm)。(4)土壤容重深层(20—40 cm)显著大于表层(P0.05),并随海拔梯度逐步增加,且林分间差异较大。(5)全碳(Total carbon, TC)、全氮(Total nitrogen, TN)、全磷(Total phosphorus, TP)含量表层显著高于深层。TC、TN随海拔升高先增后降低,TP则随海拔逐步降低。不同林分间土壤养分差异较明显。(6)结构方程模型分析得到海拔、土层、容重直接影响细根生物量,细根生物量直接影响土壤养分。林分类型通过土壤容重间接影响细根生物量。因此,林分和海拔通过影响土壤微环境而影响到细根生物量及其空间分布格局。     

The effect of fire on nutrients in a pine forest soil

The effect of a hot summer fire on soil nutrient contents in the upper 2 cm of Aleppo pine forest with a dense woody understory was studied from September 1985 to May 1986. In comparison with the adjacent unburned forest, total nitrogen decreased by 25% but available forms of nitrogen were much higher. In burned and unburned soils there was a similar trend to increase and decrease in NH ₄ ⁺ −N, However, while (NO ₂ ⁻ +NO ₃ ⁻ −N decreased in the unburned soil it rose rapidly in the burned ash soil. Total phosphorus increased by 300% after the fire but decreased again 2 months later. Also water-soluble P increased up to November and then decreased to the levels of the unburned soils. The same was true for electrical conductivity and pH, increasing immediately after the fire and then leveling off again. This increase in nutrient levels in the “ash soil” was reflected in the striking increase in shoot and root biomass and in the content of N, P, Mg, K, Ca, Zn and Fe in wheat and clover plants grown in pots in these soils. These nutrient levels were much higher in the wheat plants, which also produced 12 times more seeds in the “ash soil.” It seems that fire in these pine forests causes a short-term flush of the mineral elements in the upper “ash soil” layer which is reverted gradually via the herbaceous post-fire to the ecosystem.     

云雾山典型草原火烧不同恢复年限土壤化学性质变化

云雾山典型草原处于黄土高原半干旱地区,也是草原火灾多发区,试验比较了未烧地与新烧地、火烧后3 a和火烧后11 a土壤有机碳(SOC)、全N、全P和速效K含量的变化过程。测量的土壤深度为50 cm,每10 cm一层,比较了4个样地0—10 cm、10—20 cm、20—30 cm、30—40 cm、40—50 cm土壤养分的变化。结果表明:(1)新烧地土壤剖面各层SOC、全N、全P和速效K含量都显著高于未烧地。(2)火烧后3 a样地土壤剖面各层SOC、全N、全P和速效K含量与未烧地差异不显著。(3)火烧后11 a样地土壤剖面各层全N含量都显著高于未烧地,SOC、全P和速效K含量除了0—10 cm层与未烧地差异不显著外,其它土层均显著增加。(4)4个样地的土壤剖面各层从上到下SOC、土壤全N、全P和速效K含量呈递减趋势。(5)3个火烧样地土壤表层(0—10 cm)的pH值和未烧地差异不显著。     

Leaf‐cutting ants,seasonal burning and nutrient distribution in Cerrado vegetation

Abstract Fire and herbivory are known to modify plant community structure. Many studies have suggested that fire ashes may increase soil nutrients in dystrophic soils. Herbivores may also change plant community structure through direct effects of herbivory and affecting nutrient cycling. Leaf‐cutting ants were traditionally viewed as herbivores, although their role may be more complex, because their nests affect both chemical and physical soil properties, thus affecting plants indirectly. We investigated the effects of frequent burning and of leaf‐cutting ants on the nutrient status of an herbaceous and a shrub species occurring in the Brazilian Cerrado, a habitat that is characterized by natural burnings. The proximity of ant nests resulted in an increase of nutrients in the leaves of both vegetation strata, whereas burning sometimes resulted in a decrease of nutrients. Our results do not lead to a possible positive effect of fire on plant nutrient content. On the other hand, ant nests may represent an important source of nutrients for plants on the nutrient‐depleted Cerrado soils and may accelerate vegetation recovery after burning.     

Ash as a phosphorus fertilizer to reed canary grass: effects of nutrient and heavy metal composition on plant and soil

Fertilization effects and risks of heavy metal enrichment were studied in a field experiment, in which plots of reed canary grass (RCG) were treated annually with three different fertilizers: Ash from co‐combustion of RCG and municipal wastes (mixed ash), pure RCG ash, and commercial fertilizer (control). RCG ash is a waste product that is currently expensive to dispose of. The amounts of nutrients applied annually were 100 kg ha^?1 N, 15 kg ha^?1 P, and 80 kg ha^?1 K in all treatments. In the ash treatments, all P derived from ash, whereas N and part of the K were supplemented by fertilizers. The amount of heavy metals exceeded the limits set by the Swedish Environmental Protection Agency for all elements analyzed in the mixed ash and for Ni and Cr in the RCG ash. There were no significant differences between treatments in terms of RCG dry matter yield obtained at harvest in spring, or in heavy metal concentrations in the biomass. Soil samples from 0–5 cm, 5–10 cm, and 10–20 cm below the surface showed significant differences between treatments for the concentration of Cd, Cr, Cu, Pb, and Zn, with higher concentrations in plots fertilized with mixed ash than in the control. Neither spring yield nor soil available P was reduced by using ash instead of mineral P fertilizer, suggesting that pure RCG ash can be used to complement commercial fertilizer, albeit less frequently than here. However, ash derived from co‐combusting RCG with different waste materials (mixed ash treatment) should not be used in RCG production due to the high heavy metal content.     

Phosphorus cycling in a small watershed in the Brazilian Cerrado: impacts of frequent burning

Plant productivity in many tropical savannas is phosphorus limited. The biogeochemical cycling of P in these ecosystems, however, has not been well quantified. In the present study, we characterized P stocks and fluxes in a well-preserved small watershed in the Brazilian Cerrado. As the Cerrado is also a fire-dominated ecosystem, we measured the P stocks and fluxes in a cerrado stricto sensu plot with complete exclusion of fire for 26 years (unburned plot) and then tested some predictions about the impacts of fire impacts on P cycling in an experimental plot that was burned three times since 1992 (burned plot). The unburned area is an ecosystem with large soil stocks of total P (1,151 kg ha^?1 up to 50 cm depth), but the largest fraction is in an occluded form. Readily extractable P was found up to 3 m soil depth suggesting that deep soil is more important to the P cycle than has been recognized. The P stock in belowground biomass (0?C800 cm) was 9.9 kg ha^?1. Decomposition of fine litter released 0.97 kg P ha^?1 year^?1. Fluxes of P through bulk atmospheric deposition, throughfall and litter leachate were very low (0.008, 0.006 and 0.028 kg ha^?1 year^?1, respectively) as was stream export (0.001 kg ha^?1 year^?1). Immobilization of P by microbes during the rainy season seems to be an important mechanism of P conservation in this ecosystem. Fire significantly increased P flux in litter leachate to 0.11 kg ha^?1 year^?1, and added 1.2 kg ha^?1 of P in ash deposition after fire. We found an increase of P concentration in soil solution at 100 cm depth (from 0.03 ??g l^?1 in unburned plot to 0.3 ??g l^?1 in the burned plot). In surface soils (0?C10 cm) of the burned plot, fire decreased the concentrations of extractable organic-P fractions, but did not significantly increase inorganic-P fractions. The reduction of extractable soil organic P in the burned plot in topsoil and the increase of P in the soil solution at greater depths indicated a reduction of P availability and may increase P fixation in deep soils. Repeated fire events over the long term may result in significant net loss of available forms of phosphorus from this ecosystem.     

Gains and losses in soil nutrients associated with harvesting and burning eucalypt rainforest

In mixed eucalypt/rainforest in southern Tasmania, samples of surface soil 0 to 2 cm, 2 to 5 cm, and 5 to 10 cm were taken from a clear-felled coupe before and after burning in 1982, from a similar coupe after burning in 1979, and from an uncut area adjacent to each coupe. Factors compared were bulk density; total organic C, N, P, Ca, Mg, and K; pH; exchangeable Ca, Mg, and K; cation exchange capacity; extractable P; and N-mineralisation rates. The effect of burning was found to be restricted mainly to the upper 2 cm of soil. The combustion of organic matter caused losses of 7360 kg organic C and 211 kg N/ha; 348 kg Ca and 282 kg Mg and 151 kg K/ha were added to the soil in ash. Burning caused significant increases in pH, exchangeable Ca, Mg, and K, and in extractable P; cation exchange capacity was reduced. In the 6 months after burning only K was leached from the upper 2 cm of soil. Equilibrium levels of NH₄?N increased initially after the fire, but between 6 and 18 months, equilibrium levels and rate of production of NH₄?N during anaerobic incubation in soil of burned coupes differed little from that in adjacent uncut forest. Rates of production of NO₃?N during aerobic incubation were very low throughout the period of study. It is concluded that for soils developed on dolerite in mixed eucalypt/rainforest, a single regeneration burn probably improves the nutritional status of the soil. Nutrients lost from the area as particulate ash are in quantities that will probably be replaced in rainfall in 15 to 20 years.