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N Pools (n + pool)
Selected AbstractsPhosphorus and nitrogen in a monomictic freshwater lake: employing cyanobacterial bioreporters to gain new insights into nutrient bioavailabilityFRESHWATER BIOLOGY, Issue 6 2010OSNAT GILLOR Summary 1. It is an uncontested paradigm that an adequate supply of the macronutrients nitrogen (N) and phosphorus (P) is critical for maintaining phytoplankton primary production in aquatic ecosystems; it has also been suggested that there is an optimal total N : total P ratio for this globally significant process. 2. This ratio, normally assessed by chemical determination of the major dissolved N and P species, poses a dilemma: do chemical measurements actually reflect the bioavailable fraction of these nutrient pools? Accurate determination of the various N and P species and their fluxes into phytoplankton cells is notoriously difficult. 3. To provide a possible solution to this difficulty, we engineered strains of the cyanobacterium Synechococcus sp. strain PCC 7942 that ,report' on N and P bioavailability via a bioluminescent signal. These strains were used to quantify, for the first time, bioavailable concentrations of these essential macronutrients in a freshwater lake. 4. Only a small fraction (0.01,1%) of the chemically determined P may actually be bioavailable to this unicellular cyanobacterium and, by inference, to the phytoplankton community in general. In contrast, bioavailable N comprises most of the dissolved N pool. Consequently, bioavailable N : P ratios based on these assays are higher then those based on chemical determinations, indicating that P limitation in Lake Kinneret is more extensive then previously thought. [source] Plant and microbial N acquisition under elevated atmospheric CO2 in two mesocosm experiments with annual grassesGLOBAL CHANGE BIOLOGY, Issue 2 2005Shuijin Hu Abstract The impact of elevated CO2 on terrestrial ecosystem C balance, both in sign or magnitude, is not clear because the resulting alterations in C input, plant nutrient demand and water use efficiency often have contrasting impacts on microbial decomposition processes. One major source of uncertainty stems from the impact of elevated CO2 on N availability to plants and microbes. We examined the effects of atmospheric CO2 enrichment (ambient+370 ,mol mol,1) on plant and microbial N acquisition in two different mesocosm experiments, using model plant species of annual grasses of Avena barbata and A. fatua, respectively. The A. barbata experiment was conducted in a N-poor sandy loam and the A. fatua experiment was on a N-rich clayey loam. Plant,microbial N partitioning was examined through determining the distribution of a 15N tracer. In the A. barbata experiment, 15N tracer was introduced to a field labeling experiment in the previous year so that 15N predominantly existed in nonextractable soil pools. In the A. fatua experiment, 15N was introduced in a mineral solution [(15NH4)2SO4 solution] during the growing season of A. fatua. Results of both N budget and 15N tracer analyses indicated that elevated CO2 increased plant N acquisition from the soil. In the A. barbata experiment, elevated CO2 increased plant biomass N by ca. 10% but there was no corresponding decrease in soil extractable N, suggesting that plants might have obtained N from the nonextractable organic N pool because of enhanced microbial activity. In the A. fatua experiment, however, the CO2 -led increase in plant biomass N was statistically equal to the reduction in soil extractable N. Although atmospheric CO2 enrichment enhanced microbial biomass C under A. barbata or microbial activity (respiration) under A. fatua, it had no significant effect on microbial biomass N in either experiment. Elevated CO2 increased the colonization of A. fatua roots by arbuscular mycorrhizal fungi, which coincided with the enhancement of plant competitiveness for soluble soil N. Together, these results suggest that elevated CO2 may tighten N cycling through facilitating plant N acquisition. However, it is unknown to what degree results from these short-term microcosm experiments can be extrapolated to field conditions. Long-term studies in less-disturbed soils are needed to determine whether CO2 -enhancement of plant N acquisition can significantly relieve N limitation over plant growth in an elevated CO2 environment. [source] Linkages between plant functional composition, fine root processes and potential soil N mineralization ratesJOURNAL OF ECOLOGY, Issue 1 2009Dario A. Fornara Summary 1Plant functional composition may indirectly affect fine root processes both qualitatively (e.g. by influencing root chemistry) and quantitatively (e.g. by influencing root biomass and thus soil carbon (C) inputs and the soil environment). Despite the potential implications for ecosystem nitrogen (N) cycling, few studies have addressed the linkages between plant functional composition, root decay, root detritus N dynamics and soil N mineralization rates. 2Here, using data from a large grassland biodiversity experiment, we first show that plant functional composition affected fine root mass loss, root detritus N dynamics and net soil N mineralization rates through its effects on root chemistry rather than on the environment of decomposition. In particular, the presence of legumes and non-leguminous forbs contributed to greater fine root decomposition which in turn enhanced root N release and net soil N mineralization rates compared with C3 and C4 grasses. 3Second, we show that all fine roots released N immediately during decomposition and showed very little N immobilization regardless of plant composition. As a consequence, there was no evidence of increased root or soil N immobilization rates with increased below-ground plant biomass (i.e. increased soil C inputs) even though root biomass negatively affected root decay. 4Our results suggest that fine roots represent an active soil N pool that may sustain plant uptake while other soil N forms are being immobilized in microbial biomass and/or sequestered into soil organic matter. However, fine roots may also represent a source of recalcitrant plant detritus that is returned to the soil (i.e. fine roots of C4 and C3 grasses) and that can contribute to an increase in the soil organic matter pool. 5Synthesis. An important implication of our study is that the simultaneous presence of different plant functional groups (in plant mixtures) with opposite effects on root mass loss, root N release and soil N mineralization rates may be crucial for sustaining multiple ecosystem services such as productivity and soil C and N sequestration in many N-limited grassland systems. [source] Temperature functions of the rate coefficients of net N mineralization in sandy arable soils.JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, Issue 4 2004Part I. Derivation from laboratory incubations Abstract This study aimed to experimentally determine adequate temperature functions for the rate coefficients of net N mineralization in sandy arable soils from NW Germany. Long-term laboratory incubations were carried out in seven sandy arable soils at 3°C, 10°C, 19°C, 28°C, and 35°C in order to derive the rate coefficients of a simultaneous two-pool first-order kinetic equation. Thereby we differentiated between a small, fast mineralizable N pool, comprising mainly fresh residues, and a larger, slowly mineralizable N pool of old, humified organic matter. The rate coefficients were plotted against temperature, and fits of several different functions were tested: Arrhenius, Q10, and multiple non-mechanistic equations. The two derived rate coefficients showed very different temperature functions. Especially in critical temperature ranges (<5/10°C, >30/35°C) common Q10 functions failed to fit well, and, only below 10°C, the Arrhenius functions were in agreement with mean measured rate coefficients. Over the studied temperature range, only relatively complex, multiple equations could adequately account for the observed patterns. In addition, temperature functions that have been derived earlier from loess soils from NW Germany were found not to be transferable to the sandy arable soils studied. Thus, the results strongly question the use of the same Arrhenius or Q10 function or the same rate modifying factor for different N pools as well as for different soils as is generally done in models. Evaluations with field measurements of net N mineralization in part II of the paper (Heumann and Böttcher, 2004) will show which functions perform best in the field. Die Temperaturfunktionen der Reaktionskoeffizienten der N-Nettomineralisation in sandigen Ackerböde nI. Ableitung aus Laborinkubationen Untersuchungsziel war die experimentelle Bestimmung adäquater Temperaturfunktionen für die Reaktionskoeffizienten der N-Nettomineralisation in sandigen Ackerböden NW-Deutschlands. Anhand von Langzeit-Laborinkubationen bei 3, 10, 19, 28 und 35,°C wurden für sieben sandige Ackerböden die Reaktionskoeffizienten zweier N-Pools mit Reaktionskinetik erster Ordnung ermittelt. Dadurch konnte zwischen einem kleineren, schnell mineralisierbaren N-Pool, der hauptsächlich frische Residuen umfasst, und einem größeren, langsam mineralisierbaren N-Pool aus überwiegend alter humifizierter organischer Substanz unterschieden werden. Die ermittelten Reaktionskoeffizienten wurden gegen die Temperatur aufgetragen und verschiedene Funktionen angepasst: Arrhenius-, Q10 - und multiple nicht-mechanistische Gleichungen. Die Temperaturfunktionen der beiden Reaktionskoeffizienten unterschieden sich stark. Besonders innerhalb kritischer Temperaturbereiche (<5/10,°C, >30/35,°C) war die Übereinstimmung üblicher Q10 -Funktionen schlecht, und nur unterhalb von 10,°C stimmten die Arrhenius-Funktionen mit den mittleren gemessenen Reaktionskoeffizienten überein. Über den gesamten untersuchten Temperaturbereich konnten nur relativ komplexe, multiple Gleichungen die beobachteten Verläufe angemessen nachzeichnen. Weiterhin waren die Temperaturfunktionen, die ehemals an norddeutschen Lössböden ermittelt wurden, nicht auf die untersuchten sandigen Ackerböden übertragbar. Daher stellen die Ergebnisse den Gebrauch derselben Arrhenius- oder Q10 -Funktion sowie gleicher Ratenfaktoren für verschiedene N-Pools und auch für verschiedene Böden stark in Frage. In Teil II der Arbeit (Heumann and Böttcher, 2004) wird anhand einer Überprüfung mit Messungen der N-Nettomineralisation im Feld gezeigt, welche Funktionen die beste Übereinstimmung im Freiland erbringen. [source] Effect of the nitrification inhibitor nitrapyrin on the fate of nitrogen applied to a soil incubated under laboratory conditionsJOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, Issue 4 2003M. Kaleem Abbasi Abstract The aim of this study was to examine the effect of the nitrification inhibitor nitrapyrin on the fate and recovery of fertilizer nitrogen (N) and on N mineralization from soil organic sources. Intact soil cores were collected from a grassland field. Diammonium phosphate (DAP) and urea were applied as N sources. Cores were equilibrated at ,5 kPa matric potential and incubated at 20,°C for 42 to 56 days. Changes in NH4+ -N, accumulation of NO3, -N, apparent recovery of applied N, and emission of N2O (acetylene was used to block N2O reductase) were examined during the study. A significant increase in NH4+ -N released through mineralization was recorded when nitrapyrin was added to the control soil without N fertilizer application. In the soils to which N was added either as urea or DAP, 50,90,% of the applied N disappeared from the NH4+ -N pool. Some of this N (8,16,%) accumulated as NO3, -N, while a small proportion of N (1,%) escaped as N2O. Addition of nitrapyrin resulted in a decrease and delay of NH4+ -N disappearance, accumulation of much lower soil NO3, -N contents, a substantial reduction in N2O emissions, and a 30,40,% increase in the apparent recovery of added N. The study indicates that N recovery can be increased by using the nitrification inhibitor nitrapyrin in grassland soils at moisture condition close to field capacity. No translation. [source] Use of labelled nitrogen to measure gross and net rates of mineralization and microbial activity in permanent pastures following fertilizer applications at different time intervals,RAPID COMMUNICATIONS IN MASS SPECTROMETRY, Issue 23 2002David J. Hatch Measurements of some of the main internal N-cycling processes in soil were obtained by labelling the inorganic N pool with the stable isotope of nitrogen (15N). The 15N mean pool dilution technique, combined with other field measurements, enabled gross and net N-mineralization rates to be resolved in grassland soils, which had previously either received fertilizer N (F), or had remained unfertilized (U) for many years. The two soils were subdivided into plots that received N at different time intervals (over 3 weeks), prior to 15N measurements being made. By this novel approach, possible ,priming' effects over time were investigated to try to overcome some of the temporal problems of isotopic labelling of soil N (native plus fertilizer) and to identify possible changes in a range of primary N-transformation processes. The results suggested that an overall stimulation of microbially mediated processes occurred with all N treatments, but there were inconsistencies associated with the release of N, both in the timing and the degree to which different processes responded to the application of fertilizer N. The rates of these processes were, however, within the range of previously reported data and the 15N measurements were not adversely affected by the differences in N pools created by the treatments. Thus, the mean pool dilution technique was shown to be applicable to agricultural soils, under conditions relevant to grass swards receiving fertilizer. For example, between the,U and F treatments, the size of inorganic N pools increased by five-fold and gross rates of mineralization reached 3.5 and 4.8,µg N g,1 (dry soil) d,1, respectively, but did not vary greatly with the timing of N applications. A correlation (r2,=,0.57) was found between soil respiration (which is relatively simple to measure) and net mineralization (which is more time consuming), suggesting that the former might be used as an indicator of the latter. Although this relationship was stronger in previously unfertilized soils, the similarities found with fertilized soils suggest that this approach could be used to obtain information of wider agronomic value and would, therefore, warrant further work under a range of soil conditions. Copyright © 2002 John Wiley & Sons, Ltd. [source] Shrub expansion stimulates soil C and N storage along a coastal soil chronosequenceGLOBAL CHANGE BIOLOGY, Issue 7 2010STEVEN T. BRANTLEY Abstract Expansion of woody vegetation in grasslands is a worldwide phenomenon with implications for C and N cycling at local, regional and global scales. Although woody encroachment is often accompanied by increased annual net primary production (ANPP) and increased inputs of litter, mesic ecosystems may become sources for C after woody encroachment because stimulation of soil CO2 efflux releases stored soil carbon. Our objective was to determine if young, sandy soils on a barrier island became a sink for C after encroachment of the nitrogen-fixing shrub Morella cerifera, or if associated stimulation of soil CO2 efflux mitigated increased litterfall. We monitored variations in litterfall in shrub thickets across a chronosequence of shrub expansion and compared those data to previous measurements of ANPP in adjacent grasslands. In the final year, we quantified standing litter C and N pools in shrub thickets and soil organic matter (SOM), soil organic carbon (SOC), soil total nitrogen (TN) and soil CO2 efflux in shrub thickets and adjacent grasslands. Heavy litterfall resulted in a dense litter layer storing an average of 809 g C m,2 and 36 g N m,2. Although soil CO2 efflux was stimulated by shrub encroachment in younger soils, soil CO2 efflux did not vary between shrub thickets and grasslands in the oldest soils and increases in CO2 efflux in shrub thickets did not offset contributions of increased litterfall to SOC. SOC was 3.6,9.8 times higher beneath shrub thickets than in grassland soils and soil TN was 2.5,7.7 times higher under shrub thickets. Accumulation rates of soil and litter C were highest in the youngest thicket at 101 g m,2 yr,1 and declined with increasing thicket age. Expansion of shrubs on barrier islands, which have low levels of soil carbon and high potential for ANPP, has the potential to significantly increase ecosystem C sequestration. [source] Initial cultivation of a temperate-region soil immediately accelerates aggregate turnover and CO2 and N2O fluxesGLOBAL CHANGE BIOLOGY, Issue 8 2006A. STUART GRANDY Abstract The immediate effects of tillage on protected soil C and N pools and on trace gas emissions from soils at precultivation levels of native C remain largely unknown. We measured the response to cultivation of CO2 and N2O emissions and associated environmental factors in a previously uncultivated U.S. Midwest Alfisol with C concentrations that were indistinguishable from those in adjacent late successional forests on the same soil type (3.2%). Within 2 days of initial cultivation in 2002, tillage significantly (P=0.001, n=4) increased CO2 fluxes from 91 to 196 mg CO2 -C m,2 h,1 and within the first 30 days higher fluxes because of cultivation were responsible for losses of 85 g CO2 -C m,2. Additional daily C losses were sustained during a second and third year of cultivation of the same plots at rates of 1.9 and 1.0 g C m,2 day,1, respectively. Associated with the CO2 responses were increased soil temperature, substantially reduced soil aggregate size (mean weight diameter decreased 35% within 60 days), and a reduction in the proportion of intraaggregate, physically protected light fraction organic matter. Nitrous oxide fluxes in cultivated plots increased 7.7-fold in 2002, 3.1-fold in 2003, and 6.7-fold in 2004 and were associated with increased soil NO3, concentrations, which approached 15 ,g N g,1. Decreased plant N uptake immediately after tillage, plus increased mineralization rates and fivefold greater nitrifier enzyme activity, likely contributed to increased NO3, concentrations. Our results demonstrate that initial cultivation of a soil at precultivation levels of native soil C immediately destabilizes physical and microbial processes related to C and N retention in soils and accelerates trace gas fluxes. Policies designed to promote long-term C sequestration may thus need to protect soils from even occasional cultivation in order to preserve sequestered C. [source] Temperature functions of the rate coefficients of net N mineralization in sandy arable soils.JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, Issue 4 2004Part I. Derivation from laboratory incubations Abstract This study aimed to experimentally determine adequate temperature functions for the rate coefficients of net N mineralization in sandy arable soils from NW Germany. Long-term laboratory incubations were carried out in seven sandy arable soils at 3°C, 10°C, 19°C, 28°C, and 35°C in order to derive the rate coefficients of a simultaneous two-pool first-order kinetic equation. Thereby we differentiated between a small, fast mineralizable N pool, comprising mainly fresh residues, and a larger, slowly mineralizable N pool of old, humified organic matter. The rate coefficients were plotted against temperature, and fits of several different functions were tested: Arrhenius, Q10, and multiple non-mechanistic equations. The two derived rate coefficients showed very different temperature functions. Especially in critical temperature ranges (<5/10°C, >30/35°C) common Q10 functions failed to fit well, and, only below 10°C, the Arrhenius functions were in agreement with mean measured rate coefficients. Over the studied temperature range, only relatively complex, multiple equations could adequately account for the observed patterns. In addition, temperature functions that have been derived earlier from loess soils from NW Germany were found not to be transferable to the sandy arable soils studied. Thus, the results strongly question the use of the same Arrhenius or Q10 function or the same rate modifying factor for different N pools as well as for different soils as is generally done in models. Evaluations with field measurements of net N mineralization in part II of the paper (Heumann and Böttcher, 2004) will show which functions perform best in the field. Die Temperaturfunktionen der Reaktionskoeffizienten der N-Nettomineralisation in sandigen Ackerböde nI. Ableitung aus Laborinkubationen Untersuchungsziel war die experimentelle Bestimmung adäquater Temperaturfunktionen für die Reaktionskoeffizienten der N-Nettomineralisation in sandigen Ackerböden NW-Deutschlands. Anhand von Langzeit-Laborinkubationen bei 3, 10, 19, 28 und 35,°C wurden für sieben sandige Ackerböden die Reaktionskoeffizienten zweier N-Pools mit Reaktionskinetik erster Ordnung ermittelt. Dadurch konnte zwischen einem kleineren, schnell mineralisierbaren N-Pool, der hauptsächlich frische Residuen umfasst, und einem größeren, langsam mineralisierbaren N-Pool aus überwiegend alter humifizierter organischer Substanz unterschieden werden. Die ermittelten Reaktionskoeffizienten wurden gegen die Temperatur aufgetragen und verschiedene Funktionen angepasst: Arrhenius-, Q10 - und multiple nicht-mechanistische Gleichungen. Die Temperaturfunktionen der beiden Reaktionskoeffizienten unterschieden sich stark. Besonders innerhalb kritischer Temperaturbereiche (<5/10,°C, >30/35,°C) war die Übereinstimmung üblicher Q10 -Funktionen schlecht, und nur unterhalb von 10,°C stimmten die Arrhenius-Funktionen mit den mittleren gemessenen Reaktionskoeffizienten überein. Über den gesamten untersuchten Temperaturbereich konnten nur relativ komplexe, multiple Gleichungen die beobachteten Verläufe angemessen nachzeichnen. Weiterhin waren die Temperaturfunktionen, die ehemals an norddeutschen Lössböden ermittelt wurden, nicht auf die untersuchten sandigen Ackerböden übertragbar. Daher stellen die Ergebnisse den Gebrauch derselben Arrhenius- oder Q10 -Funktion sowie gleicher Ratenfaktoren für verschiedene N-Pools und auch für verschiedene Böden stark in Frage. In Teil II der Arbeit (Heumann and Böttcher, 2004) wird anhand einer Überprüfung mit Messungen der N-Nettomineralisation im Feld gezeigt, welche Funktionen die beste Übereinstimmung im Freiland erbringen. [source] Soil N transformations after application of 15N-labeled biomass in incubation experiments with repeated soil drying and rewettingJOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, Issue 2 2004Hans-Werner Olfs Abstract The effects of repeated soil drying and rewetting on microbial biomass N (Nbio) and mineral N (Nmin) were measured in incubation experiments simulating typical moisture and temperature conditions for soils from temperate climates in the post-harvest period. After application of in vitro15N-labeled fungal biomass to a silty loam, one set of soils was exposed to two drying-rewetting cycles (treatment DR; 14 days to decrease soil moisture to 20,% water-holding capacity (WHC) and subsequently 7 days at 60,% WHC). A control set (treatment CM) was kept at constant moisture conditions (60,% WHC) throughout the incubation. Nbio and Nmin as well as the 15N enrichment of these N pools were measured immediately after addition of 15N-labeled biomass (day 0) and after each change in soil moisture (day 14, 21, 35, 42). Drying and rewetting (DR) resulted in higher Nmin levels compared to CM towards the end of the incubation. Considerable amounts of Nbio were susceptible to mineralization as a result of soil drying (i.e., drying enhanced the turnover of Nbio), and significantly lower Nbio values were found for DR at the end of each drying period. Immediately after biomass incorporation into the soil (day 0), 22,% of the applied 15N was found in the Nmin pool. Some of this 15Nmin must have been derived from dead cells of the applied microbial biomass as only about 80,% of the microbes in the biomass suspension were viable, and only 52,% of the 15Nbio was extractable (using the fumigation-extraction method). The increase in 15Nmin was higher than for unlabeled Nmin, indicating that added labeled biomass was mineralized with a higher rate than native biomass during the first drying period. Overall, the effect of drying and rewetting on soil N turnover was more pronounced for treatment DR compared to CM during the second drying-rewetting cycle, resulting in a higher flush of mineralization and lower microbial biomass N levels. Stickstoffumsatz im Boden nach Applikation 15N-markierter Biomasse in Inkubationsversuchen mit wiederholten Trocknungs-Wiederbefeuchtungszyklen Der Einfluss wiederholter Bodentrocknung und -wiederbefeuchtung auf mikrobiellen Biomasse-N (Nbio) und mineralischen N (Nmin) wurde in Inkubationsversuchen untersucht. Bodenfeuchte und -temperatur wurden entsprechend den typischen Bedingungen in der Nachernte-Periode gemäßigter Klimazonen simuliert. Nach Applikation von in-vitro15N-markierter Biomasse zu einem Krumenboden (schluffiger Lehm) wurde eine Hälfte der Inkubationsgefäße zwei Trocknungs-Wiederbefeuchtungs-Zyklen ausgesetzt (Behandlung DR, d. h., innerhalb von 14 Tagen Absenkung der Bodenfeuchte auf 20,% der Wasserhaltekapazität (WHC) und danach 7 Tage bei 60,% WHC). Die Vergleichsgefäße wurden konstant bei 60,% der WHC inkubiert (Behandlung CM). Nbio und Nmin sowie die 15N-Anreicherung dieser N-Pools wurden sofort nach der Applikation der 15N-markierten Biomasse (Tag 0) und nach jeder Änderung in der Bodenfeuchte (Tag 14, 21, 35, 42) gemessen. Trocknung und Wiederbefeuchtung (DR) resultierte in höheren Nmin -Gehalten im Vergleich zu CM gegen Ende der Inkubation. Bei Bodentrocknung unterlagen höhere Biomasse-Anteile der Mineralisation (d. h., Trocknung forcierte den Umsatz von Nbio), so dass jeweils am Ende der Trocknungsperiode in DR niedrigere Nbio -Gehalte gefunden wurden. Sofort nach der Einarbeitung der Biomasse in den Boden (Tag 0) wurde 22,% des applizierten 15N im Nmin -Pool gefunden. Ein Teil dieses 15Nmin dürfte von bereits toten Zellen der eingesetzten Mikroben-Biomasse stammen, da nur ca. 80,% der Mikroorganismen in der verwendeten Biomasse-Suspension als lebend eingestuft werden konnte und nur 52,% des 15Nbio mittels Fumigations-Extraktions-Methode extrahierbar war. Aus dem deutlicheren Anstieg im 15Nmin im Vergleich zum unmarkierten Nmin kann geschlossen werden, dass während der ersten Trocknungsperiode zugesetzte markierte Biomasse mit einer höheren Rate als bodenbürtige Biomasse mineralisiert wurde. Insgesamt war der Effekt des Trocknens und der Wiederbefeuchtung auf den N-Umsatz im Boden für die Behandlung DR im Vergleich zu CM im zweiten Zyklus ausgeprägter. Dies zeigt sich in einem höheren Mineralisationsschub und in einem niedrigeren Gehalt an Biomasse zum Ende der Inkubation. [source] What are the effects of nitrogen deficiency on growth components of lettuce?NEW PHYTOLOGIST, Issue 3 2000M. R. BROADLEY Relationships between nitrogen (N) content and growth are routinely measured in plants. This study determined the effects of N on the separate morphological and physiological components of plant growth, to assess how N-limited growth is effected through these components. Lettuce (Lactuca sativa) plants were grown hydroponically under contrasting N-supply regimes, with the external N supply either maintained continuously throughout the period of study, or withdrawn for up to 14 d. Richards' growth functions, selected using an objective curve-fitting technique, accounted for 99.0 and 99.1% of the variation in plant dry weight for control and N-limited plants respectively. Sublinear relationships occurred between N and relative growth rates under restricted N-supply conditions, consistent with previous observations. There were effects of treatment on morphological and physiological components of growth. Leaf weight ratio increased over time in control plants and decreased in N- limited plants. Shoot:root ratio followed a similar pattern. On a whole-plant basis, assimilation of carbon decreased in N-limited plants, a response paralleled by differences in stomatal conductance between treatments. Changes in C assimilation, expressed as a function of stomatal conductance to water vapour, suggest that the effects of N limitation on growth did not result directly from a lack of photosynthetic enzymes. Relationships between plant N content and components of growth will depend on the availability of different N pools for remobilization and use within the plant. [source] Effects of Drought on the Competitive Interference of an Early Successional Species (Rubus fruticosus) on Fagus sylvatica L. Seedlings: 15N Uptake and Partitioning, Responses of Amino Acids and other N CompoundsPLANT BIOLOGY, Issue 3 2002M. N. Fotelli Abstract: We assessed the role of water availability as a factor regulating the ability of beech seedlings to cope with competitive interference for nitrogen resources by an early successional species (Rubus fruticosus). A glasshouse experiment was performed with two levels of interference (beech with and without R. fruticosus) and three levels of irrigation (high, intermediate, none). 15N uptake and partitioning of both species, and composition of N pools in leaves, roots and phloem of beech, were determined. Under all irrigation regimes, 15N uptake by beech seedlings decreased when grown together with R. fruticosus. R. fruticosus had higher 15N uptake rates than beech, under all water supply levels. When irrigation was reduced, a substantial decrease in 15N uptake of beech seedlings and a concurrent increase in 15N uptake by R. fruticosus were observed. Interference by R. fruticosus and low irrigation also affected the 15N partitioning in beech seedlings and resulted in reduced allocation of 15N to the roots. The combination of competitive interference and lack of irrigation led to an increase in soluble non-protein N in roots and leaves of beech, due to protein degradation. This response was attributed to an increase in levels of amino acids serving as osmoprotectants under these conditions. The concentration of proline in leaves of beech was negatively correlated to shoot water potential. A competition-induced reduction of total N in leaves of beech under high and intermediate irrigation was found. These results illustrate (1) the advantage of R. fruticosus in terms of N uptake when compared to young beech, particularly under inadequate water supply, and (2) the changes in N composition of beech seedlings in order to cope with reduced soil water and interference by R. fruticosus. [source] Seasonal variations in nitrate reductase activity and internal N pools in intertidal brown algae are correlated with ambient nitrate concentrationsPLANT CELL & ENVIRONMENT, Issue 6 2007ERICA B. YOUNG ABSTRACT Nitrogen metabolism was examined in the intertidal seaweeds Fucus vesiculosus, Fucus serratus, Fucus spiralis and Laminaria digitata in a temperate Irish sea lough. Internal NO3 - storage, total N content and nitrate reductase activity (NRA) were most affected by ambient NO3 - , with highest values in winter, when ambient NO3 - was maximum, and declined with NO3 - during summer. In all species, NRA was six times higher in winter than in summer, and was markedly higher in Fucus species (e.g. 256 ± 33 nmol NO3 - min,1 g,1 in F. vesiculosus versus 55 ± 17 nmol NO3 - min,1 g,1 in L. digitata). Temperature and light were less important factors for N metabolism, but influenced in situ photosynthesis and respiration rates. NO3 - assimilating capacity (calculated from NRA) exceeded N demand (calculated from net photosynthesis rates and C : N ratios) by a factor of 0.7,50.0, yet seaweeds stored significant NO3 - (up to 40,86 µmol g,1). C : N ratio also increased with height in the intertidal zone (lowest in L. digitata and highest in F. spiralis), indicating that tidal emersion also significantly constrained N metabolism. These results suggest that, in contrast to the tight relationship between N and C metabolism in many microalgae, N and C metabolism could be uncoupled in marine macroalgae, which might be an important adaptation to the intertidal environment. [source] Use of labelled nitrogen to measure gross and net rates of mineralization and microbial activity in permanent pastures following fertilizer applications at different time intervals,RAPID COMMUNICATIONS IN MASS SPECTROMETRY, Issue 23 2002David J. Hatch Measurements of some of the main internal N-cycling processes in soil were obtained by labelling the inorganic N pool with the stable isotope of nitrogen (15N). The 15N mean pool dilution technique, combined with other field measurements, enabled gross and net N-mineralization rates to be resolved in grassland soils, which had previously either received fertilizer N (F), or had remained unfertilized (U) for many years. The two soils were subdivided into plots that received N at different time intervals (over 3 weeks), prior to 15N measurements being made. By this novel approach, possible ,priming' effects over time were investigated to try to overcome some of the temporal problems of isotopic labelling of soil N (native plus fertilizer) and to identify possible changes in a range of primary N-transformation processes. The results suggested that an overall stimulation of microbially mediated processes occurred with all N treatments, but there were inconsistencies associated with the release of N, both in the timing and the degree to which different processes responded to the application of fertilizer N. The rates of these processes were, however, within the range of previously reported data and the 15N measurements were not adversely affected by the differences in N pools created by the treatments. Thus, the mean pool dilution technique was shown to be applicable to agricultural soils, under conditions relevant to grass swards receiving fertilizer. For example, between the,U and F treatments, the size of inorganic N pools increased by five-fold and gross rates of mineralization reached 3.5 and 4.8,µg N g,1 (dry soil) d,1, respectively, but did not vary greatly with the timing of N applications. A correlation (r2,=,0.57) was found between soil respiration (which is relatively simple to measure) and net mineralization (which is more time consuming), suggesting that the former might be used as an indicator of the latter. Although this relationship was stronger in previously unfertilized soils, the similarities found with fertilized soils suggest that this approach could be used to obtain information of wider agronomic value and would, therefore, warrant further work under a range of soil conditions. Copyright © 2002 John Wiley & Sons, Ltd. [source] | ||||||||||