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Mineral N (mineral + n)

Distribution by Scientific Domains

Earth and Environmental Science	81%
Chemistry	12%

Selected Abstracts

Foraging animals create fertile patches in an Australian desert shrubland

ECOGRAPHY, Issue 5 2009
Alex I. James
Fertile patches are created and maintained by a combination of physical and biologically-mediated processes including soil disturbance by animals. We examined the creation of fertile patches by 4 vertebrates, the greater bilby Macrotis lagotis, burrowing bettong Bettongia lesueur, European rabbit Oryctolagus cuniculus, and Gould's sand goanna Varanus gouldii within dunes, ecotones, and swales in a dunefield in arid South Australia. These animals all create pits when foraging for subterranean food resources. We hypothesized that 1) the effect of pits on litter capture would vary among landscapes and animal species, 2) larger pits would trap more litter and seed, 3) pits would contain more viable seed than the surrounding matrix, and 4) the effect of pits on soil chemistry would vary among animal species, and be greater in landscapes with more finely textured soils. We found that litter was restricted almost exclusively to the pits, and was greater in pits with larger openings. Litter capture was greater in ecotones and dunes than in swales. A total of 1307 seedlings from 46 genera germinated from litter samples taken from the pits, but no seedlings emerged from samples taken from soil surrounding the pits. Foraging pits contained significantly higher levels of total C and N than surrounding soil, and total C and N concentrations were greatest in swales and lowest in dunes. Pits contained ca 55% more mineralisable N that surface soils, and pits constructed by bilbies and bettongs contained half the concentration of mineralisable N as those of rabbits and goannas. Concentrations of mineral N and mineralisable N were also greatest in the swales. Our results demonstrate the importance of animal-created pits as nutrient sinks and sites for seedling establishment, and suggest that changes in the composition of arid zone vertebrates may have resulted in profound changes to nutrient and soil dynamics in arid Australia. [source]

The inherent ,safety-net' of an Acrisol: measuring and modelling retarded leaching of mineral nitrogen

EUROPEAN JOURNAL OF SOIL SCIENCE, Issue 2 2002
D. Suprayogo
Summary The inherent features of Acrisols with their increasing clay content with depth are conducive to reducing nutrient losses by nutrient adsorption on the matrix soil surfaces. Ammonium (NH4+) and nitrate (NO3,) adsorption by a Plinthic Acrisol from Lampung, Indonesia was studied in column experiments. The peak of the H218O breakthrough occurred at 1 pore volume, whereas the median pore volumes for NH4+ and NO3, ranged from 6.4 to 6.9 and 1.1 to 1.6, respectively. The adsorption coefficients (Ka in cm3 g,1) measured were 1.81, 1.51, 1.64 and 1.47 for NH4+ and 0.03, 0.09, 0.10 and 0.17 for NO3,, respectively, in the 0,0.2, 0.2,0.4, 0.4,0.6 and 0.6,0.8 m soil depth layers. The NH4+ and NO3, adsorption coefficients derived from this study were put in to the Water, Nutrient and Light Capture in Agroforestry Systems (WaNuLCAS) model to evaluate their effect on leaching in the context of several cropping systems in the humid tropics. The resulting simulations indicate that the inherent ,safety-net' (retardation mechanism) of a shallow (0.8,1 m) Plinthic Acrisol can reduce the leaching of mineral N by between 5 and 33% (or up to 2.1 g m,2), mainly due to the NH4+ retardation factor, and that the effectiveness in reducing N leaching increases with increasing depth. However, the inherent ,safety-net' is useful only if deep-rooted plants can recover the N subsequently. [source]

Effects of 15N Split-application on Soil and Fertiliser N Uptake of Barley, Oilseed Rape and Wheat in Different Cropping Systems

JOURNAL OF AGRONOMY AND CROP SCIENCE, Issue 1 2007
K. Sieling
Abstract In intensive farming systems, farmers split up and apply the N fertilization to winter cereals and oilseed rape (OSR) at several dates to meet the need of the crop more precisely. Our objective was to determine how prior fertilizer N application as slurry and/or mineral N affects contributions of fertilizer- and soil-derived N to N uptake of barley (1997), oilseed rape (OSR; 1998) and wheat (1999). In addition, residual fertilizer N effects were observed in the subsequent crop. Since autumn 1991, slurry (none, slurry in autumn, in spring, in autumn plus in spring) and mineral N fertilizer (0, 12 and 24 g N m,2) were applied annually. Each year, the treatments were located on the same plots. In 1997,1999, the splitting rates of the mineral N fertilization were labelled with 15N. Non-fertilizer N uptake was estimated from the total N uptake and the fertilizer 15N uptake. All three crops utilized the splitting rates differently depending on the time of application. Uptake of N derived from the first N rate applied at the beginning of spring growth was poorer than that from the second splitting rate applied at stem elongation (cereals) or third splitting rate applied at ear emergence or bud formation (all three crops). In contrast, N applied later in the growing season was taken up more quickly, resulting in higher fertilizer N-use efficiency. Mineral N fertilization of 24 g N m,2 increased significantly non-fertilizer N uptake of barley and OSR at most of the sampling dates during the growing season. In cereals, slurry changed the contribution of non-fertilizer N to the grain N content only if applied in spring, while OSR utilized more autumn slurry N. In OSR and wheat, only small residual effects occurred. The results indicate that 7 years of varying N fertilization did not change the contribution of soil N to crop N uptake. [source]

Effect of Different Crop Densities of Winter Wheat on Recovery of Nitrogen in Crop and Soil within the Growth Period

JOURNAL OF AGRONOMY AND CROP SCIENCE, Issue 3 2001
K. Blankenau
Previous experiments have shown that, at harvest of winter wheat, recovery of fertilizer N applied in early spring [tillering, Zadok's growth stage (GS) 25] is lower than that of N applied later in the growth period. This can be explained by losses and immobilization of N, which might be higher between GS 25 and stem elongation (GS 31). It was hypothesized that a higher crop density (i.e. more plants per unit area) results in an increased uptake of fertilizer N applied at GS 25, so that less fertilizer N is subject to losses and immobilization. Different crop densities of winter wheat at GS 25 were established by sowing densities of 100 seeds m,2 (Slow), 375 seeds m,2 (Scfp= common farming practice) and 650 seeds m,2 (Shigh) in autumn. The effect of sowing density on crop N uptake and apparent fertilizer N recovery (aFNrec = N in fertilized treatments , N in unfertilized treatments) in crops and soil mineral N (Nmin), as well as on lost and immobilized N (i.e. non-recovered N = N rate , aFNrec), was investigated for two periods after N application at GS 25 [i.e. from GS 25 to 15 days later (GS 25 + 15d), and from GS 25 + 15d to GS 31] and in a third period between GS 31 and harvest (i.e. after second and third N applications). Fertilizer N rates varied at GS 25 (0, 43 and 103 kg N ha,1), GS 31 (0 and 30 kg N ha,1) and ear emergence (0, 30 and 60 kg ha,1). At GS 25 + 15d, non-recovered N was highest (up to 33 kg N ha,1 and up to 74 kg N ha,1 at N rates of 43 and 103 kg N ha,1, respectively) due to low crop N uptake after the first N dressing. Non-recovered N was not affected by sowing density. Re-mineralization during later growth stages indicated that non-recovered N had been immobilized. N uptake rates from the second and third N applications were lowest for Slow, so non-recovered N at harvest was highest for Slow. Although non-recovered N was similar for Scfp and Shigh, the highest grain yields were found at Scfp and N dressings of 43 + 30 + 60 kg N ha,1. This combination of sowing density and N rates was the closest to common farming practice. Grain yields were lower for Shigh than for Scfp, presumably due to high competition between plants for nutrients and water. In conclusion, reducing or increasing sowing density compared to Scfp did not reduce immobilization (and losses) of fertilizer N and did not result in increased fertilizer N use efficiency or grain yields. Einfluß unterschiedlicher pflanzendichten von Winterweizen auf die Wiederfindung von Stickstoff in Pflanze und Boden während der Vegetationsperiode Aus Wintergetreideversuchen ist bekannt, daß zur Ernte die Wiederfindung von Düngerstickstoff aus der Andüngung (Bestockung, [GS-Skala nach Zadok] GS 25) im Aufwuchs und in mineralischer Form im Boden (Nmin) niedriger ist als die von Düngerstickstoff der Schosser-und Ährengaben. Dies kann auf höhere Verluste bzw. eine höhere Immobilisation von Düngerstickstoff zwischen GS 25 und Schoßbeginn zurückgeführt werden, da hier die N-Aufnahme der Pflanzen im Vergleich zu späteren Wachstumsstadien gering ist. Daraus wurde abgeleitet, daß eine Erhöhung der Pflanzendichte zu einer erhöhten Aufnahme von früh gedüngtem N führen könnte, so daß weniger Dünger-N für Verlust- und Immobilisationsprozesse im Boden verbleibt. Unterschiedliche Pflanzendichten wurden durch unterschiedliche Aussaatstärken im Herbst erreicht (Slow= 100 Körner m,2, Scfp [herkömmliche Praxis]= 375 Körner m,2, Shigh= 650 Körner m,2). In der folgenden Vegetationsperiode wurde der Einfluß der verschiedenen Aussaatstärken auf die N-Aufnahme, die apparente Wiederfindung von Dünger-N (aFNrec = N in gedüngten , N in ungedüngten Prüfgliedern) in Pflanzen und Nmin, sowie auf potentielle Verluste und Immobilisation von Dünger-N (N-Defizit = N-Düngung , aFNrec) für zwei Phasen im Zeitraum zwischen der ersten N-Gabe (GS 25) und der Schossergabe zu GS 31 (d. h. zwischen GS 25 und 15 Tagen später [GS 25 + 15d] und von GS 25 + 15d bis GS 31), sowie zwischen GS 31 und der Ernte (d. h. nach der zweiten und dritten N-Gabe) untersucht. Die N-Düngung variierte zu den Terminen GS 25 (0, 43, 103 kg N ha,1), GS 31 (0, 30 kg N ha,1) und zum Ährenschieben (0, 30, 60 kg N ha,1). Unabhängig von der Aussaatstärke war das N-Defizit zum Termin GS 25 + 15d am höchsten (bis zu 33 kg N ha,1 und 74 kg N ha,1 bei einer N-Düngung von 43 bzw. 103 kg N ha,1), da die N-Aufnahme durch die Pflanzen während der Bestockungsphase am geringsten war. Das N-Defizit zeigt vornehmlich immobilisierten N an, da zu späteren Terminen eine Re-Mobilisation von N auftrat. Zwischen GS 31 und der Ernte wurden für die Aussaatstärke Slow die geringsten Aufnahmeraten von Düngerstickstoff aus der Schosser- und Ährengabe errechnet, so daß für Slow die höchsten N-Defizitmengen ermittelt wurden. Obwohl die N-Defizitmengen für Scfp und Shigh annähernd gleich waren, wurden bei N-Düngung von 43 + 30 + 60 kg N ha,1 für Scfp die höchsten Kornerträge erzielt. Diese Kombination von Aussaatstärke und N-Düngung kann als praxisüblich bezeichnet werden. Für Shigh wurden vermutlich niedrigere Kornerträge erzielt, weil die Konkurrenz um Nährstoffe und Wasser zwischen den Pflanzen aufgrund der hohen Pflanzendichte am intensivsten war. Die Ergebnisse lassen den Schluß zu, daß eine Verringerung oder Erhöhung der Pflanzendichte über entsprechende Aussaatstärken nicht zu einer Reduktion der Dünger-N-Immobilisation (oder von N-Verlusten) führt und demnach auch nicht die Dünger-N-Ausnutzung durch die Bestände erhöht wird. [source]

Labile soil organic carbon, soil fertility, and crop productivity as influenced by manure and mineral fertilizers in the tropics

JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, Issue 5 2010
Siba Prasad Datta
Abstract In recent years, organic agriculture has been receiving greater attention because of the various problems like deterioration in soil health and environmental quality under conventional chemical-intensive agriculture. However, little information is available on the comparative study related to the impact of use of mineral fertilizers and organic manures on the soil quality and productivity. A long-term field experiment was initiated in 2001 to monitor some of the important soil-quality parameters and productivity under soybean,wheat crop rotation. The treatments consisted of 0, 30, and 45,kg N ha,1 for soybean and of 0, 120, and 180,kg N ha,1 for wheat. The entire amount of N was supplied to both the crops through urea and farmyard manure (FYM) alone or in combination at 1:1 ratio. Results indicated that Walkley-and-Black C (WBC; chromic acid,oxidizable) exhibited a marginal increase under only organic treatments as compared to control treatment (without fertilizers and manure) after completion of five cropping cycles. In case of labile-C (KMnO4 -oxidizable) content in soil, relatively larger positive changes were recorded under organic, mixed inputs (integrated) and mineral fertilizers as compared to WBC. Maximum improvement in the values of C-management index (CMI), a measure of soil quality was recorded under organic (348,362), followed by mixed inputs (268,322) and mineral fertilizers (198,199) as compared to the control treatment after completion of five cropping cycles. Similarly there was a substantial increase in KCl-extractable N; in Olsen-P; as well as in DTPA-extractable Zn, Fe, and Mn under organic treatments. Although labile soil C positively contributed to the available N, P, K, Zn, Fe, and Mn contents in soil, it did not show any relationship with the grain yield of wheat. After completion of the sixth cropping cycle, organic treatments produced 23% and 39% lower grain yield of wheat as compared to that under urea-treated plots. Relatively higher amount of mineral N in soil at critical growth stages and elevated N content in plant under mineral-fertilizer treatments compared to FYM treatments were responsible for higher yield of wheat under mineral fertilizers. [source]

Effects of two contrasting agricultural land-use practices on nitrogen leaching in a sandy soil of Middle Germany

JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, Issue 3 2009
Christian Böhm
Abstract The objective of this study is to evaluate different agricultural land-use practices in terms of N leaching and to give recommendations for a sustainable agriculture on sandy soils in Middle Germany. Soil mineral N (Nmin) and leachate N were quantified at a sandy soil in N Saxony during 3 years. Two treatments were applied: intensive (I),using inorganic and organic fertilizer and pesticides, and organic (O),exclusively using organic fertilizer, legume-based crop rotation, and no pesticides. Split application of mineral fertilizers did not result in substantial N losses at treatment I. Legumes induced a considerable increase of soil mineral N and particularly of leachate mineral N (Nmin_perc) at treatment O. High Nmin_perc concentrations (up to 78 mg N L,1) were observed during as well as after the cultivation of legumes. These high Nmin_perc concentrations are the reason why clearly higher Nmin_perc losses were determined at treatment O (62 kg N ha,1 y,1) compared to treatment I (23,kg N ha,1 y,1). At both treatments, the quantity of N losses was strongly affected by the precipitation rates. Concentrations and losses of dissolved organic N (DONperc) were assessed as above average at both treatments. The results suggest that the DONperc concentration is influenced by precipitation, soil coverage, and organic fertilizers. Higher values were determined in the percolation water of treatment O. The average annual DONperc losses amounted to 15,kg N ha,1 at I and to 32 kg N ha,1 at O. The average monthly percentage of DONperc losses on the loss of the dissolved total N of percolation water (DTNperc) ranged between <1% and 55% at O and between 2% and 56% at I. For the whole measuring period of 29 months, the relative amounts of DONperc of DTNperc (21% at O and 25% at I) were more or less the same for both treatments. The results show that DONperc can contribute significantly to the total N loss, confirming the importance to consider this N fraction in N-leaching studies. It was concluded that at sandy sites, a split application of mineral fertilizers, as applied at treatment I, seems to be more expedient for limiting the N leaching losses than legume-based crop rotations. [source]

Organic fertilizers derived from plant materials Part II: Turnover in field trials

JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, Issue 2 2006
Torsten Müller
Abstract Our aim was to investigate two different organic fertilizers derived from plant materials (OFDP) with respect to their nitrogen (N) and carbon (C) turnover in field trials planted with small radish (Raphanus sativus L. var. sativus) and white cabbage (Brassica oleracea L. convar. capitata var. alba) or fallow. The two fertilizers investigated were coarse seed meal of yellow lupin (Lupinus luteus L.) and coarse meal of castor cake (Ricinus communis L.). Under cool spring conditions, the soil turnover of yellow lupin,seed meal was slightly enhanced compared to castor-cake meal. During the vegetation period of the vegetables, N added with both fertilizers was metabolized more or less completely by soil microorganisms. Due to similar efficiencies of the fertilizers tested, no significant difference could be found in the N uptake of plants. From this point of view, yellow lupin,seed meal, which can be produced by farmers themselves, has the potential to replace the widely used castor-cake meal. Considerable amounts of N may remain in the field after fertilization with OFDPs either as mineral N or as easily mineralizable organic N. This N should be utilized immediately by a succeeding crop to avoid leaching losses. [source]

Soil- and plant-based nitrogen-fertilizer recommendations in arable farming

JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, Issue 4 2005
Hans-Werner Olfs
Abstract Under- as well as overfertilization with nitrogen (N) will result in economic loss for the farmer due to reduced yields and quality of the products. Also from an ecological perspective, it is important that the grower makes the correct decision on how much and when to apply N for a certain crop to minimize impacts on the environment. To aggravate the situation, N is a substance that is present in many compartments in different forms (nitrate, ammonium, organic N, etc.) in the soil-plant environment and takes part in various processes (e.g., mineralization, immobilization, leaching, denitrification, etc.). Today, many N-recommendation systems are mainly based on yield expectation. However, yields are not stable from year to year for a given field. Also the processes that determine the N supply from other sources than fertilizer are not predictable at the start of the growing season. Different methodological approaches are reviewed that have been introduced to improve N-fertilizer recommendations for arable crops. Many soil-based methods have been developed to measure soil mineral N (SMN) that is available for plants at a given sampling date. Soil sampling at the start of the growing period and analyzing for the amount of NO -N (and NH -N) is a widespread approach in Europe and North America. Based on data from field calibrations, the SMN pool is filled up with fertilizer N to a recommended amount. Depending on pre-crop, use of organic manure, or soil characteristics, the recommendation might be modified (±10,50,kg N ha,1). Another set of soil methods has been established to estimate the amount of N that is mineralized from soil organic matter, plant residues, and/or organic manure. From the huge range of methods proposed so far, simple mild extraction procedures have gained most interest, but introduction into practical recommendation schemes has been rather limited. Plant-analytical procedures cover the whole range from quantitative laboratory analysis to semiquantitative "quick" tests carried out in the field. The main idea is that the plant itself is the best indicator for the N supply from any source within the growth period. In-field methods like the nitrate plant sap/petiole test and chlorophyll measurements with hand-held devices or via remote sensing are regarded as most promising, because with these methods an adequate adjustment of the N-fertilizer application strategy within the season is feasible. Prerequisite is a fertilization strategy that is based on several N applications and not on a one-go approach. Boden- und Pflanzenanalyse zur Stickstoff-Düngebedarfsprognose in Ackerkulturen Unter- und Überdüngung mit N führen zu deutlichen ökonomischen Verlusten für Landwirte, da sowohl der Ertrag als auch die Qualität der Erzeugnisse vermindert werden. Auch aus ökologischer Sicht ist die richtige Entscheidung des Anbauers über Höhe und Zeitpunkt der N-Düngung von Bedeutung, um die Auswirkungen auf die Umwelt so gering wie möglich zu halten. Erschwerend kommt hinzu, dass N in sehr vielen Umweltkompartimenten in verschiedenen Bindungsformen (Nitrat, Ammonium, organisch gebundener N) vorkommt und dass N in verschiedenste Umsetzungsprozesse involviert ist (Mineralisation, Immobilisation, Auswaschung, Denitrifikation). Auch heutzutage orientieren sich viele Systeme, die zur N-Düngebedarfsprognose eingesetzt werden, im Wesentlichen an der Ertragserwartung. Dabei ist jedoch zu bedenken, dass weder der Ertrag als von Jahr zu Jahr stabil angesehen werden kann, noch dass die Prozesse, die das bodenbürtige N-Angebot bestimmen, zu Beginn der Vegetationsperiode hinreichend gut vorausgesagt werden können. Daher werden im Folgenden verschiedene methodische Ansätze erläutert, die zur Verbesserung der N-Düngebedarfsprognose für Ackerkulturen geeignet erscheinen. Viele Bodenanalyse-Methoden zielen darauf ab, den mineralischen N-Vorrat des Bodens, der an einem bestimmten Beprobungstermin als pflanzenverfügbarer N vorliegt, zu erfassen. Die Bodenprobeentnahme zu Beginn der Vegetationsperiode und die Bestimmung der Menge an Nitrat (und Ammonium) ist ein in Europa und Nord-Amerika weitverbreiteter Ansatz. Anhand der Daten aus Kalibrierversuchen kann dann abgeleitet werden, wie viel Dünger-N zum Auffüllen des N-Vorrats eingesetzt werden soll. In Abhängigkeit von Vorfrucht, Einsatz von Wirtschaftsdüngern oder weiteren Bodeneigenschaften kann diese Empfehlung modifiziert werden (± 10 bis 50,kg N ha,1). Weitere Bodenuntersuchungsmethoden wurden entwickelt, um die Menge des während der Vegetationszeit aus der organischen Bodensubstanz, aus Ernteresten und/oder aus Wirtschaftsdüngern mineralisierten N zu bestimmen. Obwohl aus der Vielzahl der vorgeschlagenen Methoden einfache "milde" Extraktionsverfahren eine gewisse Bedeutung erlangt haben, werden diese in der Praxis bei der Ermittlung des N-Düngebedarfs als zusätzliche Information nur selten berücksichtigt. Verfahren der Pflanzenanalyse umfassen einen weiten Bereich von quantitativen Laboranalysen bis zu halbquantitativen Schnelltests, die direkt auf dem Acker eingesetzt werden können. Die wesentliche Idee beim Einsatz der Pflanzenanalyse ist die Vorstellung, dass die Pflanze an sich der beste Indikator ist, die N-Verfügbarkeit aus den verschiedenen Quellen gewissermaßen kumulativ innerhalb der Wachstumszeit anzuzeigen. Methoden, die auf dem Acker eingesetzt werden können, wie z.,B. der Nitrat-Pflanzensaft- (oder Blattstiel-)Test sowie die Chlorophyll-Messung mit Handgeräten oder berührungslose Messverfahren haben den klaren Vorteil, dass sie eine schnelle Anpassung der N-Düngestrategie während der Vegetation ermöglichen. Voraussetzung dazu ist allerdings, dass die N-Düngestrategie nicht auf einer Einmal-Applikation beruht, sondern dass die N-Düngermenge auf mehrere Teilgaben verteilt wird. [source]

Soil N transformations after application of 15N-labeled biomass in incubation experiments with repeated soil drying and rewetting

JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, Issue 2 2004
Hans-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]

Soil biochemical and chemical changes in relation to mature spruce (Picea abies) forest conversion and regeneration

JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, Issue 3 2003
Zheke Zhong
Abstract To investigate soil changes from forest conversion and regeneration, soil net N mineralization, potential nitrification, microbial biomass N, L-asparaginase, L-glutaminase, and other chemical and biological properties were examined in three adjacent stands: mature pure and dense Norway spruce (Picea abies (L.) Karst) (110 yr) (stand I), mature Norway spruce mixed with young beech (Fagus sylvatica) (5 yr) (stand II), and young Norway spruce (16 yr) (stand III). The latter two stands were converted or regenerated from the mature Norway spruce stand as former. The studied soils were characterized as having a very low pH value (2.9 , 3.5 in 0.01 M CaCl2), a high total N content (1.06 , 1.94,%), a high metabolic quotient (qCO2) (6.7 , 16.9 g CO2 kg,1 h,1), a low microbial biomass N (1.1 , 3.3,% of total N, except LOf1 at stand III), and a relatively high net N mineralization (175 , 1213 mg N kg,1 in LOf1 and Of2, 4 weeks incubation). In the converted forest (stand II), C,:,N ratio and qCO2 values in the LOf1 layer decreased significantly, and base saturation and exchangeable Ca showed a somewhat increment in mineral soil. In the regenerated forest (stand III), the total N storage in the surface layers decreased by 30,%. The surface organic layers (LOf1, Of2) possessed a very high net N mineralization (1.5 , 3 times higher than those in other two stands), high microbial biomass (C, N), and high basal respiration and qCO2 values. Meanwhile, in the Oh layer, the base saturation and the exchangeable Ca decreased. All studied substrates showed little net nitrification after the first period of incubation (2 weeks). In the later period of incubation (7 , 11 weeks), a considerable amount of NO3 -N accumulated (20 , 100,% of total cumulative mineral N) in the soils from the two pure spruce stands (I, III). In contrast, there was almost no net NO3 -N accumulation in the soils from the converted mixed stand (II) indicating that there was a difference in microorganisms in the two types of forest ecosystems. Soil microbial biomass N, mineral N, net N mineralization, L-asparaginase, and L-glutaminase were correlated and associated with forest management. Chemische und biochemische Veränderungen der Bodeneigenschaften durch Verjüngung und Waldumbau eines Fichtenaltbestandes Um die durch den Waldumbau und die Regeneration bedingten Standortsveränderungen zu untersuchen, wurden die Netto-Stickstoffmineralisierung, die potenzielle Nitrifikation, der mikrobiell gebundene Stickstoff (Nmic), L-Asparaginase, L-Glutaminase sowie weitere chemische und biologische Parameter an drei benachbarten Standorten untersucht: Standort I, reiner Fichtenaltbestand (Picea abies (L.) Karst ,110 Jahre); Standort II, Fichtenaltbestand mit Buchenunterbau (Fagus sylvatica , 5 Jahre); Standort III, reine Fichtenaufforstung (16 Jahre). Die Standorte II und III entstanden infolge des Waldumbaus aus reinen Fichtenaltbeständen. Die untersuchten Böden sind gekennzeichnet durch sehr niedrige pH-Werte (pH(H2O) 3, 7 , 4, 2, pH (CaCl2) 2, 9 , 3, 5), hohe Gesamtstickstoffgehalte (1, 06 , 1, 94,%), hohe metabolische Quotienten (6, 7,16, 9g CO2 kg,1 h,1), geringe Nmic -Gehalte (1, 1 , 3, 3,% des Gesamt-N, ausgenommen LOf1 von Standort III) und eine relativ hohe N-Nettomineralisation (175 , 1213 mg N Kg,1 in LOf1 und Of2, nach 4 Wochen Inkubation). Am Standort II nahm das C,:,N-Verhältnis und der qCO2 im LOf1 -Horizont deutlich ab, wohingegen der Gehalt an austauschbarem Ca sowie die Basensättigung im Mineralboden geringfügig zunahmen. Am Standort III nahm der N-Vorrat (Auflagehumus + Mineralboden 0 , 10,cm) um 30,% ab. In den LOf1 - und Of2 -Lagen des Auflagehumus dieses Standortes traten eine hohe N-Nettomineralisation (1, 5- bis 3fach höher als in den Standorten I und II), hohe Gehalte an mikrobiell gebundenem C und N, eine erhöhte Basalatmung sowie erhöhte qCO2 -Werte auf. In den Oh-Lagen hingegen nahm die Basensättigung ab. Alle untersuchten Standorte zeigten in der ersten Periode der Inkubation (0 bis 2 Wochen) eine geringe Netto-Nitrifikation. An den Standorten I und III fand in der späteren Periode (7. bis 11. Woche) eine Anreicherung an NO3 (20 , 100,% des gesamten mineralischen N-Vorrates) statt. Im Gegensatz dazu wurde am Standort II keine NO3 -N- Anreicherung festgestellt. Dies deutet auf einen Unterschied in der Zusammensetzung der mikrobiellen Gemeinschaften in den zwei verschiedenen Forstökosystemen hin. Nmic, N-Nettomineralisation, L-Asparaginase und L-Glutaminase korrelieren miteinander und zeigen eine enge Beziehung zu den Bewirtschaftungsformen. [source]

Contribution of dissolved organic nitrogen to N leaching from four German agricultural soils

JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, Issue 6 2002
Jan Siemens
Abstract Dissolved organic nitrogen (DON) substantially contributes to N leaching from forest ecosystems. However, little is known about the role of DON for N leaching from agricultural soils. Therefore, the aim of our study was to quantify the contribution of DON to total N leaching from four agricultural soils. Concentrations and fluxes of DON and mineral N were monitored at two cropped sites (Plaggic Anthrosols) and two fallow plots (Plaggic Anthrosol and Gleyic Podzol) from November 1999 till May 2001 by means of glass suction plates. The experimental sites were located near the city of Münster, NW Germany. Median DON concentrations in 90 cm depth were 2.3 mg l,1 and 2.0 mg l,1 at the cropped sites and 1.6 mg l,1 and 1.3 mg l,1 at the fallow sites. There was only a slight (Anthrosols) or no (Gleyic Podzol) decrease in median DON concentrations with increasing depth. Total N seepage was between 19 kg N ha,1 yr,1 and 46 kg N ha,1 yr,1 at the fallow sites and 16,159 kg N ha,1 yr,1 at the cropped sites. For the fallow plots, DON seepage contributed 10,21,% to the total N flux (4,5 kg DON ha,1 yr,1), at the cropped sites DON seepage was 6,21,% of the total N flux (6,10 kg DON ha,1 yr,1). Thus, even in highly fertilized agricultural soils, DON is a considerable N carrier in seepage that should be considered in detailed soil N budgets. Beitrag von gelöstem organisch gebundenen Stickstoff zur N-Auswaschung aus vier deutschen landwirtschaftlich genutzten Böden Während viele Studien die Bedeutung der Auswaschung von gelöstem organisch gebundenen Stickstoff (DON) für N-Verluste aus Waldökosystemem zeigen, existieren nur wenige Daten zur DON-Auswaschung aus landwirtschaftlich genutzten Böden. Das Ziel unserer Studie war es deshalb, den Beitrag von DON zur Auswaschung von N aus vier landwirtschaftlichen Böden zu quantifizieren. Von November 1999 bis Mai 2001 erfassten wir die Konzentrationen und Flüsse von DON und mineralischem Stickstoff auf zwei bewirtschafteten Flächen (Plaggenesche) und zwei Bracheflächen (Plaggenesch und Gley-Podsol) mit Hilfe von Glassaugplatten. Die Untersuchungsflächen befanden sich nahe Münster/Westfalen. Der Median der DON-Konzentrationen in 90 cm Bodentiefe betrug auf den bewirtschafteten Flächen 2.3 mg l,1 und 2.0 mg l,1, auf den Brachen 1.6 mg l,1 und 1.3 mg l,1. Wir stellten nur eine geringe Abnahme (Plaggenesche) oder keine Abnahme (Gley-Podsol) des Medians der DON-Konzentration mit der Tiefe fest. Die Gesamt-N-Auswaschung lag zwischen 19 kg N ha,1 a,1 und 46 kg N ha,1 a,1 für die Bracheflächen und zwischen 16 kg N ha,1 a,1 und 156 kg N ha,1 a,1 für die bewirtschafteten Flächen. Im Falle der Bracheflächen machte DON 10,21,% (4,5 kg DON ha,1 a,1) der Gesamt-N-Auswaschung aus. Dieser Anteil betrug 6,21,% (6,10 kg DON ha,1 a,1) für die bewirtschafteten Flächen. Auch in intensiv gedüngten landwirtschaftlichen Böden ist die Auswaschung von DON also ein wichtiger Austragspfad für N und sollte deshalb in detaillierten N-Bilanzen berücksichtigt werden. [source]

Nitrogen release dynamics and transformation of slow release fertiliser products and their effects on tea yield and quality

JOURNAL OF THE SCIENCE OF FOOD AND AGRICULTURE, Issue 5 2008
Dr Wen-Yan Han
Abstract BACKGROUND: Tea (Camellia sinensis (L.) O. Kuntze) is a perennial leaf harvested crop. It requires more nitrogen than most other crops and preferentially utilises NH4+ to NO3, when both are available in the soil. It is expected that slow release fertilisers coupled with a nitrification inhibitor could improve the N use efficiency and simultaneously reduce environmental pollution. In this study, three slow release fertilisers were developed and tested: CaMg phosphate coated urea with dicyandiamide (DCD) as a nitrification inhibitor and polyolefin coated urea with and without DCD. The main aim was to compare the nitrogen release dynamics and transformation of these fertilisers and their effects on tea yield and quality. RESULTS: The results showed that the coatings significantly slowed N release and kept mineral N in soils at a higher concentration for a longer time compared to uncoated urea. Polyolefin was a superior coating to CaMg phosphate. DCD was an effective nitrification inhibitor and significantly reduced the ratio of nitrate to total mineral N in a highly acidic tea soil. The 15N use efficiency was 29% where uncoated fertiliser was applied and 46% where polyolefin coated fertiliser with DCD was applied. The application of slow release fertilisers increased the chlorophyll content in mature leaves and enhanced the uptake of mineral elements by tea plants. Bud sprouting, shoot growth and mature leaf longevity were significantly improved, resulting in higher biomass of tea plants. Slow release fertilisers increased the yield of shoots by 51,143% (mean, 106%) in a pot experiment and 4,14% (mean, 9%) in a field experiment compared to uncoated urea. Tea quality parameters, especially free amino acids, were also significantly increased. CONCLUSION: Slow release fertilisers, especially polyolefin coated urea with DCD could significantly increase the N use efficiency and improve tea growth. Their uses in tea fields not only improved the profit margin, but possibly reduced environmental pollution. Copyright © 2008 Society of Chemical Industry [source]

Changes in soil nitrogen availability due to stand development and management practices on semi-arid sandy lands, in northern China

LAND DEGRADATION AND DEVELOPMENT, Issue 5 2009
F. S. Chen
Abstract Soil nitrogen (N) availability is one of the limiting factors for plant growth on sandy lands. Little is known about impacts of afforestation on soil N availability and its components in southeastern Keerqin sandy lands, China. In this study, we measured N transformation under sandy Mongolian pine (Pinus sylvestris var. mongolica Litv.) plantations of different ages (grassland, young, middle-aged, close-to-mature) and management practices (non-grazing and free-grazing) during the growing seasons using the ion exchange resin bag method. Results showed that, for all plots and growing season, soil NH -N, NO -N, mineral N, and relative nitrification index, varied from 0·18 to 1·54, 0·96 to 22·05, 1·23 to 23·58,µg,d,1,g,1 dry resin, and 0·76 to 0·97, respectively, and NO -N dominated the available N amount due to intense nitrification in these ecosystems. In general, the four indices significantly increased in the oldest plantation, with corresponding values in non-grazing sites lower than those in free-grazing sites (p,<,0·05). Our studies indicated that it is a slow, extended process to achieve improvement in soil quality after afforestation of Mongolian pine in the study area. Copyright © 2009 John Wiley & Sons, Ltd. [source]

Long-term influence of manure and mineral nitrogen applications on plant and soil 15N and 13C values from the Broadbalk Wheat Experiment,

RAPID COMMUNICATIONS IN MASS SPECTROMETRY, Issue 11 2008
Mehmet Senbayram
The Broadbalk Wheat Experiment at Rothamsted Research in the UK provides a unique opportunity to investigate the long-term impacts of environmental change and agronomic practices on plants and soils. We examined the influence of manure and mineral fertiliser applications on temporal trends in the stable N (15N) and C (13C) isotopes of wheat collected during 1968,1979 and 1996,2005, and of soil collected in 1966 and 2000. The soil ,15N values in 1966 and 2000 were higher in manure than the mineral N supplied soil; the latter had similar or higher ,15N values than non-fertilised soil. The straw ,15N values significantly decreased in all N treatments during 1968 to 1979, but not for 1996,2005. The straw ,15N values decreased under the highest mineral N supply (192,kg,N,ha,1,year,1) by 3, from 1968 to 1979. Mineral N supply significantly increased to straw ,13C values in dry years, but not in wet years. Significant correlations existed between wheat straw ,13C values with cumulative rainfall (March to June). The cultivar Hereward (grown 1996,2005) was less affected by changes in environmental conditions (i.e. water stress and fertiliser regime) than Cappelle Desprez (1968,1979). We conclude that, in addition to fertiliser type and application rates, water stress and, importantly, plant variety influenced plant ,13C and ,15N values. Hence, water stress and differential variety response should be considered in plant studies using plant ,13C and ,15N trends to delineate past or recent environmental or agronomic changes. Copyright © 2008 John Wiley & Sons, Ltd. [source]