Soil Decomposition Rates Research Articles

Some perspectives on carbon sequestration in agriculture

One of the main options for greenhouse gas (GHG) mitigation identified by the IPCC is the sequestration of carbon in soils. Since the breaking of agricultural land in most regions, the carbon stocks have been depleted to such an extent, that they now represent a potential sink for CO 2 removal from the atmosphere. Improved management will however, be required to increase the inputs of organic matter in the top soil and/or decrease decomposition rates. In this paper we use data from selected regions to explore the global potential for carbon sequestration in arable soils. While realising that C sequestration is not limited to the selected regions, we have, however, focussed our review on two regions: (i) Canadian Prairies and (ii) The Tropics. In temperate regions, management changes for an increase in C involve increase in cropping frequency (reducing bare fallow), increasing use of forages in crop rotations, reducing tillage intensity and frequency, better crop residue management, and adopting agroforestry. In the tropics, agroforestry remains the primary method by which sequestration rates may be significantly increased. Increases in soil C may be achieved through improved fertility of cropland/pasture; on extensive systems with shifting cultivation cropped fallows and cover crops may be beneficial, and adopting agro forestry or foresting marginal cropland is also an alternative. In addition, in the tropics it is imperative to reduce the clearing of forests for conversion to cropland. Some regional analyses of soil C sequestration and sequestration potential have been performed, mainly for temperate industrialized North America where the majority of research pertaining to C sequestration has been carried out. More research is needed, especially for the Tropics, to more accurately capture the impact of region-specific interactions between climate, soil, and management of resources on C sequestration, which are lost in global level assessments. By itself, C sequestration in agricultural soils can make only modest contributions (3–6% of fossil fuel contributions) to mitigation of overall greenhouse gas emissions. However, effective mitigation policies will not be based on any single ‘magic bullet’ solutions, but rather on many modest reductions which are economically efficient and which confer additional benefits to society. In this context, soil C sequestration is a significant mitigation option.

Changes in the ratio of twig to foliage in litterfall with species composition, and consequences for decomposition across a long term chronosequence

In the past two centuries, anthropogenic fire suppression has affected many biomes, including boreal forests. Absence of fire in the boreal zone is often linked to declining soil fertility and increased carbon sequestration in the humus through changes in NPP and litter decomposition. We studied tree litterfall and litter decomposition for thirty lake islands in the boreal forested zone of Sweden, which differ naturally in fire regime: larger islands have burned far more frequently than smaller ones because they are intercepted more often by lightning. We used litter trays to show that the ratio of twig to foliar litterfall for Picea abies with prolonged absence of fire is largely responsible for the concomitant increased twig proportion in the total litterfall. We hypothesised that the increased twig proportion in the litterfall with time since fire would affect overall decomposition by reducing net litter quality and through impairing decomposition of associated foliar litters. We established a litter decomposition mesocosm experiment based on litter from the three main tree species found on the islands. From each of the thirty islands, we prepared a set of litterbags comprising three mixtures (all foliar litters combined, all twig litters combined, and all twig and foliar litters combined), plus monotypes (i.e. each of the separate foliage and twig litters for each species). Unlike most studies, we used the natural litterfall proportions in the mixtures. We found a (negative) effect of time since wildfire on decomposition rate for only the foliage‐twig mixtures, although twig litter did not inhibit the decomposition of foliar litter within these mixtures. The reduced decomposition rate in the foliage‐twig mixture from the small islands was therefore due to the increased proportion of twigs in the mixtures from these islands. Our results suggest that, with prolonged absence of fire, the increase of twig proportion in the foliage‐twig litterfall for P. abies combined with the shift to canopy dominance by P. abies may be important in contributing to reduced decomposition rates in boreal forest soils.

Decomposition rates of buried substrates increase with altitude in the forest-alpine tundra ecotone

Decomposition rates were measured across the forest-alpine tundra ecotone on two mountains in the Colorado Front Range. Cotton strips decomposed in the surface soils of forest, krummholz, and tundra plots for one year. We expected decomposition rates to decline with altitude or be most rapid in the krummholz. Surprisingly, decomposition rates increased from forest to tundra on Mt. Evans and remained constant across the ecotone on Niwot Ridge, highlighting differences in biogeochemical processes between two nearby mountains with otherwise similar alpine and subalphine ecosystems. Our results support the concept that decomposition rates exhibit a curvilinear relationship with soil temperature and moisture. However, soil moisture was found to be the primary factor controlling cellulose decomposition rates in soils in the forest-alpine tundra ecotone. Cellulose decomposition rates increased with soil depth indicating greater microbial activity in the mineral soil than in the organic horizon due to greater soil moisture. In addition to microbial activity, decomposition rates in the tundra may be enhanced by physical degradation from freeze-thaw events and vigorous root growth.

La neve come fattore di rilievo nel determinare lo stock di carbonio nel suolo

Abstract: Based on recent experimental evidence, a comment is made on the importance of snow depth in controlliing soil temperature and decomposition rate of soil organic matter, with special reference to mountain ecosystems.

Simulated changes in vegetation distribution, land carbon storage, and atmospheric CO2 in response to a collapse of the North Atlantic thermohaline circulation

It is investigated how abrupt changes in the North Atlantic (NA) thermohaline circulation (THC) affect the terrestrial carbon cycle. The Lund–Potsdam–Jena Dynamic Global Vegetation Model is forced with climate perturbations from glacial freshwater experiments with the ECBILT-CLIO ocean–atmosphere–sea ice model. A reorganisation of the marine carbon cycle is not addressed. Modelled NA THC collapses and recovers after about a millennium in response to prescribed freshwater forcing. The initial cooling of several Kelvin over Eurasia causes a reduction of extant boreal and temperate forests and a decrease in carbon storage in high northern latitudes, whereas improved growing conditions and slower soil decomposition rates lead to enhanced storage in mid-latitudes. The magnitude and evolution of global terrestrial carbon storage in response to abrupt THC changes depends sensitively on the initial climate conditions. These were varied using results from time slice simulations with the Hadley Centre model HadSM3 for different periods over the past 21 kyr. Changes in terrestrial storage vary between −67 and +50 PgC for the range of experiments with different initial conditions. Simulated peak-to-peak differences in atmospheric CO2 are 6 and 13 ppmv for glacial and late Holocene conditions. Simulated changes in δ13C are between 0.15 and 0.25‰. These simulated carbon storage anomalies during a NA THC collapse depend on their magnitude on the CO2 fertilisation feedback mechanism. The CO2 changes simulated for glacial conditions are compatible with available evidence from marine studies and the ice core CO2 record. The latter shows multi-millennial CO2 variations of up to 20 ppmv broadly in parallel with the Antarctic warm events A1 to A4 in the South and cooling in the North.

Paludification and management of forested peatlands in Canada: a literature review

The Clay Belt region of Quebec and Ontario supports a large forest resource and an important forest industry. In this region, the majority of the harvested volume allotted to forest companies is in forested peatlands and boreal forests prone to paludification. Paludification is the accumulation of organic matter over time, and is generally believed to be caused by increasing soil moisture and Sphagnum colonization. Paludification is influenced by external and internal factors; it reduces soil temperature, decomposition rates, microbial activity, and nutrient availability. As a result, paludification may lead to lower site productivity with time after disturbance. Therefore, in harvested stands with a thick organic matter layer, low soil disturbance (as opposed to fire) and water table rise may create favourable conditions for paludification that may ultimately be detrimental to timber production. Past experiences suggest several solutions to prevent or control the negative effects of paludification. Drainage and fertilization applied together are generally good techniques to control paludification and to improve tree productivity. On the other hand, we suggest that site preparation as well as prescribed burning, preceded or not by drainage, are avenues of research that deserve to be explored because they hold the potential to control or even reverse paludification, especially where peat accumulation is caused by natural succession or where lateral peat expansion has occurred. Key words: paludification, forested peatland, productivity, wildfire, careful logging, soil disturbance.

Plant community development is affected by nutrients and soil biota

Summary Plant community development depends to a great extent on the availability of soil nutrients, but recent studies underline the role of symbiotic, herbivorous and pathogenic soil biota. We tested for interactions between these biotic and abiotic factors by studying the effects of additional nutrients and the removal of soil biota on the replacement of grassland plant species typical of different successional stages. Species representing each of the early, mid and target phases of secondary succession in a grassland community (four per phase) were grown in mid‐successional grassland soil. The mixed plant communities were grown in sterilized and non‐sterilized soil, at three nutrient supply levels. The distribution of shoot biomass over the different plant species, and the total root biomass, were determined, as well as the composition of nematode and microarthropod communities and soil decomposition rates. The effect of nutrient supply on plant community composition depended on soil sterilization. In sterilized soil, the plant community was initially dominated by grasses that increased in dominance even without fertilization. In non‐sterilized soil, the plant community was more diverse and grass dominance decreased over time, except with high fertilization. Fertilization enhanced the productivity of the plant community in sterilized and, to a greater extent, in non‐sterilized soil. The abundance of root‐feeding nematodes was positively related to increased root biomass, pointing to a strong bottom‐up control. Increased levels of nutrient supply were associated with reduced abundance of omnivorous nematodes, the cause of this reduction being less clear. Increased soil fertility altered the functional diversity of the soil nematode community, which might, in the longer term, also affect their feedback effects on the plant community. Increased nutrient supply reduced soil decomposition activity in the non‐sterilized soil, but not in the sterilized soil. Our results imply that soil biota may reduce the effects of nutrient supply on plant dominance. Incorporating the effects of soil biota on plant species interactions into studies on succession, plant species diversity and restoration may therefore considerably increase our understanding of the observed plant community patterns.

Sensitivity of a dynamic global vegetation model to climate and atmospheric CO2

AbstractThe equilibrium carbon storage capacity of the terrestrial biosphere has been investigated by running the Lund–Potsdam–Jena Dynamic Global Vegetation Model to equilibrium for a range of CO2 concentrations and idealized climate states. Local climate is defined by the combination of an observation‐based climatology and perturbation patterns derived from a 4 × CO2 warming simulations, which are linearly scaled to global mean temperature deviations, ΔTglob. Global carbon storage remains close to its optimum for ΔTglob in the range of ±3°C in simulations with constant atmospheric CO2. The magnitude of the carbon loss to the atmosphere per unit change in global average surface temperature shows a pronounced nonlinear threshold behavior. About twice as much carbon is lost per degree warming for ΔTglob above 3°C than for present climate. Tropical, temperate, and boreal trees spread poleward with global warming. Vegetation dynamics govern the distribution of soil carbon storage and turnover in the climate space. For cold climate conditions, the global average decomposition rate of litter and soil decreases with warming, despite local increases in turnover rates. This result is not compatible with the assumption, commonly made in global box models, that soil turnover increases exponentially with global average surface temperature, over a wide temperature range.

A Laboratory Incubation Method for Determining the Rate of Microbiological Degradation of Skeletal Muscle Tissue in Soil

A controlled laboratory experiment is described, in principle and practice, which can be used for the of determination the rate of tissue decomposition in soil. By way of example, an experiment was conducted to determine the effect of temperature (12 degrees, 22 degrees C) on the aerobic decomposition of skeletal muscle tissue (Organic Texel x Suffolk lamb (Ovis aries)) in a sandy loam soil. Measurements of decomposition processes included muscle tissue mass loss, microbial CO2 respiration, and muscle tissue carbon (C) and nitrogen (N). Muscle tissue mass loss at 22 degrees C always was greater than at 12 degrees C (p < 0.001). Microbial respiration was greater in samples incubated at 22 degrees C for the initial 21 days of burial (p < 0.01). All buried muscle tissue samples demonstrated changes in C and N content at the end of the experiment. A significant correlation (p < 0.001) was demonstrated between the loss of muscle tissue-derived C (Ct) and microbially-respired C (Cm) demonstrating CO2 respiration may be used to predict mass loss and hence biodegradation. In this experiment Q10 (12 degrees C-22 degrees C) = 2.0. This method is recommended as a useful tool in determing the effect of environmental variables on the rate of decomposition of various tissues and associated materials.

Mechanisms of the Priming Effect in a Savannah Soil Amended with Cellulose

Two mechanisms have been hypothesized to explain the priming effect (PE), that is, the acceleration of soil C decomposition by fresh C input to soil. First, extracellular enzymes that are produced to decompose fresh C by fresh C specialized microbes may be partly efficient in degrading soil C. Second, depending on the competition with fresh C specialized microbes, part of the fresh C may be absorbed by soil C decomposing microbes. This absorption increases the populations of soil C decomposing microbe and hence the decomposition rate of soil C. The PE was quantified in a savannah soil amended with13C‐labeled cellulose at a rate of 495 mg C kg−1Cellulase was applied to the soil at a rate of 30 000 units kg−1soil to quantify the contribution of cellulase to the PE of cellulose. The rate of soil C decomposition increased by 55% with cellulose addition leading to PE of 234 mg C kg−1Cellulase released 32 mg C‐glucose from soil cellulose, representing only 14% of the PE. This indicated that the decomposition of soil C required the production of specific enzymes, and that the PE resulted from the stimulation of microbes able to provide soil C decomposing enzymes. Our results also showed that cellulose stimulated at least two types of microbes: soil C decomposing microbes that may also use cellulose and cellulose specialized microbes that exclusively decompose cellulose. These results indicate that the PE depends on microbial competition. We estimated that, following cellulose addition, soil humus stock was depleted by 174 mg C kg−1

Simulation of terrestrial carbon cycle balance model in Tibet

Based on climate material, the simplified terrestrial carbon cycle balance (TCCB) model was established, which is semi-mechanism and semi-statistics. Through TCCB model, our estimate indicates that the southeastern part of the Tibetan Plateau has much higher carbon content, and we have calculated the litter carbon pool, NPP, carbon fluxes and described their spatial characteristics in this region. Based on the TCCB model simulation, NPP in Tibet is 1.73 X 108tC/a, soil organic input rate is 0.66 × 108 tC/a, litter mineralization rate is 1.07 × 108 tC/a, vegetation litterfall rate is 1.73 ×108tC/a, the litter carbon pool is 7.26 × 108 tC, and soil decomposition rate is 309.54 × 108 tC/a. The carbon budget was also analyzed based on the estimates of carbon pool and fluxes. The spatial distributions of carbon pools and carbon fluxes in different compartments of terrestrial ecosystem were depicted with map respectively in Tibet. The distribution of NPP, vegetation litterfall rate, litter, litter mineralization rate, soil organic input rate and the soil decomposition rate were abstracted with temperature, precipitation, fractional vegetation and land feature.

Formation and Loss of Humic Substances During Decomposition in a Pine Forest Floor

Since twice as much C is sequestered in soils as is contained in the atmosphere, the factors controlling the decomposition rate of soil C are important to the assessment of the effects of climatic change. The formation of chemically resistant humic substances might be an important process controlling recycling of CO 2 to the atmosphere. Our objectives were to measure the rate of formation and loss of humic substances during 13 yr of litter decomposition. We placed nets on the floor of a white pine (Pinus strobus) forest to separate each annual layer of litter for 13 yr and measured humic substance concentration using NaOH extraction followed by chromatographic fractionation. The humic acid fraction increased from 2.1% of the C in litterfall to 15.7% after 1 yr. On a grams per square meter (g m -2 ) basis the humic substance fraction increased during the first year and then declined, with a half decay time (t 1/2 ) of 5.1 yr, which was significantly slower than the bulk litter (t 1/2 = 3.9 yr). The carboxylic C concentration estimated from 13 C nuclear magnetic resonance (NMR) increased in the litter over time, though total mass of carboxylic acid C in the forest floor also declined over the 13-yr period (t 1/2 = 4.6 yr). While humic substances in the forest floor decomposed at a somewhat slower rate than bulk litter during Years 1 to 13, they decomposed much faster than has been calculated from 14 C dating of the refractory fraction of organic matter in the mineral soil.

Organisms, decomposition, and growth of pine seedlings in boreal forest soil affected by sod cutting and trenching

In an experiment with factorial design performed in a mature, mixed Norway spruce (Picea abies (L.) Karst.) and Scots pine (Pinus sylvestris L.) stand in central Finland, we studied the effects of sod cutting (exposing the mineral soil simulating mechanical site preparation) and trenching the study plot (excluding root-mycorrhizal connections) on soil organisms, decomposition rate and pine seedling performance. During two growing seasons after sod cutting, the growth of pine seedlings was significantly enhanced compared to plots with the organic layer left intact. Some epiedaphic soil animals, such as ants, spiders and certain entomobryid collembolan, were more active (pitfall sampling) on sod-cut plots. By the end of the second growing season numbers of enchytraeids were greater in the exposed mineral soil than in the mineral soil under the forest floor. Trenching induced changes in microbial phospholipid fatty acid (PLFA) pattern and collembolan community structure with decreased numbers of collembolans and biomass of fungi in organic soil of uncut plots. In addition, N content of pine seedlings increased after trenching. Overall, the effects of trenching on the measured variables were similar in sod-cut and uncut plots. We conclude that the effects of mechanical site preparation on decomposers and decomposition processes can be explained partly by exclusion of mycorrhizal-root connections and partly by a decrease in unfavourable conditions created by the organic soil layer and ground vegetation.

Formation and Loss of Humic Substances During Decomposition in a Pine Forest Floor

Since twice as much C is sequestered in soils as is contained in the atmosphere, the factors controlling the decomposition rate of soil C are important to the assessment of the effects of climatic change. The formation of chemically resistant humic substances might be an important process controlling recycling of CO2 to the atmosphere. Our objectives were to measure the rate of formation and loss of humic substances during 13 yr of litter decomposition. We placed nets on the floor of a white pine (Pinus strobus) forest to separate each annual layer of litter for 13 yr and measured humic substance concentration using NaOH extraction followed by chromatographic fractionation. The humic acid fraction increased from 2.1% of the C in litterfall to 15.7% after 1 yr. On a grams per square meter (g m−2) basis the humic substance fraction increased during the first year and then declined, with a half decay time (t1/2) of 5.1 yr, which was significantly slower than the bulk litter (t1/2 = 3.9 yr). The carboxylic C concentration estimated from 13C nuclear magnetic resonance (NMR) increased in the litter over time, though total mass of carboxylic acid C in the forest floor also declined over the 13-yr period (t1/2 = 4.6 yr). While humic substances in the forest floor decomposed at a somewhat slower rate than bulk litter during Years 1 to 13, they decomposed much faster than has been calculated from 14C dating of the refractory fraction of organic matter in the mineral soil.

Nutrient fluxes and growth of Carapa guianensis Aubl. in two plantation systems in the central Amazon

The K, Mg, and P fluxes as well as the growth dynamics of the important timber tree Carapa guianensis Aubl. were compared in a monoculture and in an enrichment plantation on a “terra firme” site near Manaus, central Amazon. During the 7 years experimental period, the K, Mg, and P fluxes and the balance of the soil were quantified for monthly intervals. The nutrient input into the soil was calculated from the wet and dry deposition as well as from litter decomposition. The nutrient output out of the soil was calculated from the net nutrient uptake of the vegetation and the nutrient leaching from the soil. The growth dynamics of the planted trees were studied by means of biomass data obtained from dendrometric measurements and total tree harvesting. After 7 years of growth, the K, Mg, and P balance of the soil of the enrichment plantation was stabilised, whereas a significant deficit of the K, Mg, and P balance of the soil of the monoculture became obvious, caused by high leaching of K and Mg from the soil and low litter decomposition rates. Due to strong competition during the first 5 years of growth, a reduced biomass production of the planted Carapa trees was found in the enrichment plantation compared to trees grown in the monoculture. After that period tree growth was strongly reduced in the monoculture, whereas after 7 years, growth of Carapa grown in the enrichment plantation was still steady. From this study, it was concluded that due to the balanced K, P, and Mg input and output of the soil and more sustainable growth of the planted trees in the enrichment plantation compared to the traditional monoculture, the cultivation of Carapa for timber production is recommended in diverse plantations, such as enrichment plantations on this study site.

Procedure for Determining the Biodegradation of Radiolabeled Substrates in a Calcareous Soil

Calcareous soils are frequently typified by a low availability of plant nutrients due to poor solubility of these elements at high pH. Calcicole plants have recently been shown to release organic acids in response to the nutrient deficient conditions prevailing in these soils. It has been speculated, however, that the efficiency of this nutrient mobilization mechanism may be significantly reduced by microbial degradation of the organic acids. In conventional methods, root exudate degradation is typically determined by the addition of 14C‐radiolabeled substrates to soil and subsequent tracking of their fate with time by trapping evolved 14CO2 in a strong alkali trap. However, in calcareous soils, 14CO2 and H214CO3 produced by microbial decomposition may become trapped as Ca(H14CO3)2 The aim of this study was to develop and validate an experimental procedure for the accurate quantification of 14C‐labeled substrate degradation rates in calcareous soils. Conventional methods for determining 14C‐labeled substrate decomposition rates in calcareous soils are inaccurate due to incomplete recovery of 14CO2 Up to 49% of the 14CO2 produced during microbial degradation of 14C‐labeled organic acids (malate, oxalate, citrate) was trapped as carbonate in this calcareous soil (pH 7.58). For an acid soil (pH 4.32) no detectable amount of 14CO2 was trapped. We describe a simple, accurate, and reliable method, which includes a postincubation HCl addition, for the accurate determination of 14CO2‐evolution and substrate degradation in calcareous soils.

Immobilization of soil nitrogen as a possible method for the restoration of sandy grassland

Abstract.Experiments were designed to test the applicability of nitrogen immobilization as a means of accelerating the recovery of an endemic open sandy grassland (Festucetum vaginatae danubiale) on old fields in the Great Hungarian Plain. Effects of various carbon sources (sucrose, starch, cellulose and sawdust) and their combinations in different quantities were studied in laboratory microcosms. Carbon addition decreased nitrogen availability in all cases, the intensity and timing of change being dependent on the type of carbon source applied. The combination of 2 g each of sucrose and polysaccharides (starch, cellulose, sawdust) per kg soil was found to be the most effective, as sucrose decreased available nitrogen content of soil intensively and the polysaccharides maintained the immobilized nitrogen for a longer period. In a follow‐up experiment, sucrose and sawdust were selected for field application to test their effectiveness in immobilizing N and accelerating restoration. The field experiment was established to test the importance of abiotic site differences in the immobilization of soil nitrogen. Selected sites were located along an elevation, moisture and productivity gradient. Soil organic matter, microbial biomass‐C and decomposition rate varied between sites depending on the elevation gradient. At two sites with lower soil moisture and organic matter levels carbon addition increased microbial activity and nitrogen immobilization significantly.

Decomposition rates and feeding activities of soil fauna in deciduous forest soils in relation to soil chemical parameters following liming and fertilization

This study investigated the influence of liming and P/K fertilization on the feeding activities of soil fauna and leaf litter decomposition rates in deciduous forest soils. The parameters examined were correlated to soil chemical characteristics. In 1994, we established a field experiment with six plots in an oak-beech forest and added different amounts of dolomite, partly combined with P/K fertilization. Two years thereafter a bait-lamina test was used to examine the feeding activity of soil fauna and a minicontainer test to study beech-leaf decomposition. In 1996, the feeding activity in the Ah horizon was lower in the plots left untreated in 1994 than in the plots which had been fertilized in 1994. The highest feeding activity was found in the treatment with 6 t dolomite ha–1 plus P/K. In all plots, the feeding activity decreased with increasing soil depth. The decomposition rates varied from 0.49% to 0.78% week–1 in the period April–October 1996. In 1996, the plots treated with 6 t dolomite ha–1 had the highest decomposition rates and differed significantly from those treated with 9 t or 15 t dolomite ha–1. No significant differences were found between the untreated plots and those treated with 9 t or 15 t dolomite ha–1. These results were confirmed by those obtained in 1997. The C/N ratio of litter also decreased, mostly in the treatment with 6 t dolomite ha–1. Feeding activities in the Ah horizon correlated positively with pH and concentrations of mobile Ca, Mg, K, and negatively with concentrations of mobile Al and heavy metals. We concluded that an increased supply of mobile nutrients and a decrease in mobile Al and heavy metals in these forest soils, as well as a balanced ratio between macro- and micronutrients, led to increased biological activity.

Nitrogen uptake by rhizomes of the clonal sedge Carex bigelowii: a previously overlooked nutritional benefit of rhizomatous growth

Studies on the rhizomatous clonal sedge Carex bigelowii, at a fellfield site in subarctic Swedish Lapland examined the ecological potential of rhizomes as nitrogen uptake systems. Direct application of a solution of 15NH415NO3 to the rhizomes of C. bigelowii significantly enriched the 15N content of the plant tissue. The pattern of enrichment indicated movement of labelled nitrogen into rhizomes and adjoining tissue (including roots and shoots), showing both uptake and translocation via the rhizome system. There was a gradient of decreasing 15N enrichment with increasing distance from the point of labelling, and estimation of the total mass of nitrogen taken up via labelled rhizomes showed low levels and rates of uptake. Quantification of the size of rhizome and root systems of C. bigelowii at the study site indicates that 80% of the living biomass may be below ground, and that the surface area of the rhizome system of C. bigelowii is approx. two‐thirds that of the roots. The rhizome system of C. bigelowii can therefore act as a route for nitrogen uptake, with the potential to exploit almost as great a volume of soil as the root system. This mechanism of nitrogen uptake may play an important role in the Arctic, where many species have a clonal, rhizomatous growth form. In addition, plant growth in many arctic ecosystems is limited by low soil nutrient availability, a result of low temperatures (leading to slow soil decomposition rates) and patchy resource distribution. Nitrogen uptake via rhizomes may provide plants with the capacity to take advantage of transient nutrient supplies, and may partly compensate for the cost of developing and maintaining persistent rhizome networks in ecosystems where nutrient resources are in short supply.

Isotope techniques to study phosphorus cycling in agricultural and forest soils: a review

A sound understanding of nutrient dynamics in ecosystems is required in order to manage these systems on a sustainable basis. A valuable approach to studying phosphorus (P) dynamics in soil-plant systems has been the use of P isotope techniques. Isotope techniques used for studying P cycling in agricultural and forest soils are reviewed in this paper with particular reference to advances made in the part 15 years. A brief discussion of the properties of P isotopes and their measurements is included together with techniques for measuring exchangeable P in the soil, dissolution and decomposition rates of inorganic and organic P sources applied to the soil, rates of organic P immobilization and mineralization, rates of P release and retention in the soil, root activity and lifter decomposition rates in forest soils, and gene probing and hybridization. Basic principles, assumptions, procedures, limitations and merits of methods are discussed. These techniques have served as or have the potential to be valuable tools for advancing our understanding of P dynamics in soil-plant systems, and for studying the molecular characteristics of microbial communities in relation to the cycling of nutrients in the soil.