Interactions of nitrogen fertilizers and forest humus—i fir and black pine

In incubation experiments in the laboratory interactions of urea or NH₄NO₃ with humus from stands of fir (Abies cephalonica, Loudon) growing on soils developed from flysch (shales) and limestone and with humus from stands of black pine (pinus nigra, Arn.) growing on soils developed from peridotites, limestone and schists were investigated.Fir humus from stands on flysch and limestone and black pine humus from limestone showed nitrification but it was absent from black pine humus from stands on peridotites and on schists. Humus from stands on schists showed appreciable ammonification. Increasing concentrations of urea did not initiate nitrification in the latter type of humus. No substantial N immobilization was detected in spite of relatively high P immobilization. Increases in concentration of Ca, Mg and K occurring on incubation of humus samples were related to the ability of a humus type to nitrify rather than to concentrations of added urea-N.Urea was hydrolyzed rapidly to NH⁺₄ during contact with various types of humus, resulting in an increase of pH. Production of NH⁺₄ from urea was only minimally affected by drying the humus samples at 70°C for 20 h before incubation but was reduced to 30% at 1–5°C.     

Leaching of nitrogen forms from controlled‐release nitrogen fertilizers

Abstract

Application of soluble forms of nitrogen (N) fertilizers to sandy soils may cause leaching of nitrate N (NO₃‐N) resulting in contamination of groundwater. The leaching loss of N may be reduced to a certain extent by the use of controlled‐release N formulations. A leaching column study was conducted to evaluate the leaching of urea, ammonium N (NH₄‐N), and NO₃‐N forms from selected urea‐based controlled‐release formulations (Meister, Osmocote, and Poly‐S) and uncoated urea under eight cycles of intermittent leaching and dry conditions. Following leaching of 1,760 mL of water (equivalent to 40 cm rainfall) through the soil columns, the recovery of total N (sum of all forms) in the leachate accounted for 28, 12, 6, or 5% of the total N applied as urea, Poly‐S, Meister, and Osmocote, respectively. Loss of urea‐N from all fertilizer sources was pronounced during the initial leaching events (with the exception of Meister). Cumulative leaching of urea‐N was 10% for uncoated urea while <1.7% for the controlled‐release formulations. Cumulative leaching of NH₄‐N was 6.2% for uncoated urea while <0.5% for the controlled‐release formulations. Cumulative leaching loss of NO₃‐N was 3.78% for Osmocote, 4.6% for Meister, 10.4% for urea, and 10.5% for Poly‐S. This study demonstrates a significant reduction in leaching of N forms from controlled‐release formulations as compared to that from the soluble form.     

Interactions between Escherichia coli and allophane—II. Metabolism

A purified allophane clay fraction increased the respiration of Escherichia coli (ATCC 11303B) by buffering the suspension against decreases in pH. Allophane had no significant effect on respiration in the presence of 0.02 M phosphate buffer. When E. coli was exposed to pH values below 5.0 in the presence of allophane, allophane supernatant (which contains soluble Al), or soluble Al. toxicity was evident even after raising the pH to 7.0.     

Carbon and nitrogen turnover in response to warming and nitrogen addition during early stages of forest litter decomposition—an incubation experiment

Purpose

Little is known about the interactive effects of temperature, nitrogen (N) supply, litter quality, and decomposition time on the turnover of carbon (C) and N of forest litter. The objective of this study was to investigate the interactive effects of warming, N addition and tree species on the turnover of C and N during the early decomposition stage of litters in a temperate forest.

Materials and methods

A 12-week laboratory incubation experiment was carried out. The leaf litters including two types of broadleaf litters (Quercus mongolica and Tilia amurensis), a needle litter (Pinus koraiensis), and a mixed litter of them were collected from a broad-leaved Korean pine mixed forest ecosystem in northeastern China in September 2009. Nine treatments were conducted using three temperatures (15, 25, and 35 °C) combined with three doses of N addition (equal to 0, 75, and 150 kg?·?ha^?1?a^?1, respectively, as NH₄NO₃).

Results and discussion

After 12 weeks of incubation, the mass loss ranged between 12 and 35 %. The broadleaf litters had greater mass loss and cumulative CO₂–C emission than the needle litter. Temperature and N availability interacted to affect litter mass loss and decomposition rate. The dissolved organic carbon (DOC) and nitrogen (DON) concentrations in litter leachate varied widely with litter types. DOC increased significantly with increased temperature but decreased significantly with increased N availability. DON increased significantly with increased N availability but showed a higher level at the moderate decomposition temperature. The amounts of CO₂ and N₂O emission were significantly higher at 25 °C than those at 15 and 35 °C, and were significantly increased by the N addition.

Conclusions

The present study indicated relatively intricate temperature and N addition effects on C and N cycling during early stages of litter decomposition, implying that future increases in temperature and N deposition will directly affect C and N cycling in broad-leaved Korean pine mixed forest ecosystem, and may indirectly influence the ecosystem composition, productivity, and functioning in NE China. It is, therefore, important to understand the interactive effects of biotic and abiotic factors on litter decomposition in field conditions in order to assess and predict future ecosystem responses to environmental changes in NE China.     

The effect of lime and fertilizers on four lignite overburdens under non‐drained conditions: II. Weathering.

Abstract

Four lignite overburdens from a potential lignite mining area of Louisiana were used to evaluate the effect of rates of fertilizer, lime, plant growth and simulated poor drainage conditions on the weathering of these materials. Common bermudagrass (Cynodon dactylon) grown on each overburden material in pots lined with polyethylene bags received 0, 1/2>x, 1x, 2x and 4x the recommended rate of fertilizer which was a combination of N, P and K. Lime was applied to the overburdens based on soil test lime requirement to increase the pH to 6.5.

Enrichment (fertilizers, non‐drained conditions and lime) had a significant effect on the weathering of the overburdens. The pH, EC, organic C, P, K, Ca, Mg, S, Fe, Mn, Zn, Cu, Na and Al were significantly affected by one or more of these parameters. Visual observations indicated that fertilizers stimulated root production, which effectively increased the weathering of the overburdens. Lime, applied as CaO, did not increase the pH of the Cow Bayou material substantially, suggesting the presence of pyrite, which was confirmed by X‐ray diffraction analysis. As pyrite oxidized in the Cow Bayou material, soluble salts accumulated on the surface of the material and on the lower parts of the plant. Gypsum and jarosite precipitated as the solution ionic strength of this material increased due to the weathering of the pyrite.

The Prairie Terrace overburden was selected as the best potential topsoil since it had more favorable physical and chemical characteristics which would promote successful reclamation. Reduced materials such as Cow Bayou and Naborton had undesirable physical and chemical properties. Changes in the chemical properties of these materials would be difficult to predict and soil amendments such as lime and gypsum would be needed in significant quantities for successful reclamation. Dolet Hills, a sandy material, had a less desirable texture and would require frequent irrigation and fertilization if it were used as a topsoil substitute.     

Studies of nitrogen immobilization and mineralization in calcareous soils—II: Mineralization of immobilized nitrogen from soil fractions of different particle size and density

¹⁵NO^?₃ was immobilized in a calcareous sandy soil and a calcareous clay soil each incubated with glucose and wheat straw. Net mineralization of organic-¹⁵N was more rapid in the sandy soil, irrespective of C amendment, and in soils amended with glucose. Intermittent drying and wetting of soils during incubation stimulated mineralization of ¹⁵N-labelled and native soil organic-N in all treatments. The availability (percentage mineralization) of recently-immobilized ¹⁵N consistently exceeded that of the native soil N. Ratios of the availability of labelled and unlabelled N were similar in the sandy and clay soils but varied according to C amendment, drying and wetting cycle and incubation period.Changes in the distribution of immobilized N amongst soil extracts and soil fractions of different particle size and density were determined during periods of net N mineralization. In straw-amended soils, the organic-¹⁵N of a light fraction, sp.gr. < 1.59, decomposed relatively rapidly during the late mineralization period. Decreases of organic ¹⁵N of the fine clay fraction were also recorded. In glucose-amended soils, net N mineralization was accompanied by significant decreases in the concentrations of organic-¹⁵N of the silt and fine clay fractions.Drying and rewetting of soils hastened or magnified changes occurring in the organic-¹⁵N of soil fractions, but qualitatively, the pattern of change was similar to that observed with soils incubated under uniformly-moist conditions.The percentage distribution of labelled and unlabelled N suggested that in the long term, the silt fraction will accumulate an increasing proportion of the more stable nitrogenous residues.     

Effect of nitrogen and sulphur fertilizers and seed inoculation with rhizobium phaseoli on the nitrogen‐sulphur relationships of bean (phaseolus vulgaris L.)

A greenhouse experiment with beans (Phaseolus vulgaris L.) was performed in order to investigate the effect of nitrogen and sulphur application and seed inoculation on the yield, leaf area, distribution of different nitrogen and sulphur fractions and N/S ratio in shoot, fruit and root.

Inoculation of plants together with nitrogen or sulphur application produces an increase in the concentration of total nitrogen and a decrease in the accumulation of nitrate‐nitrogen and sulphate‐sulphur in shoot, fruit and root. Leaf area increased more with nitrogen than with sulphur application while the highest amounts of fruit dry matter were obtained with sulphur application.

N: S ratios obtained were different according to the part of the plant tested. Sulphur fertilization decreased the N: S ratios in shoot, fruit and root. The data obtained indicate that and adequate N: S ratio can insure maximum production of yield.     

Studies of nitrogen immobilization and mineralization in calcareous soils—IV. Changes in the organic nitrogen of light and heavy subfractions of silt- and fine clay-size particles during nitrogen turnover

A calcareous clay nd a calcareous sand, were fractionated densimetrically by dispersion in organic liquids of sp. gr. 1.59–2.06. The N contents of the light fractions decreased with increasing densities of the suspending liquids and were up to 18–23 times higher than those of the whole soils. Light fraction organic-N of both the sandy and clay soils was obtained mainly from silt-size components. However, the efficiency, with which light fraction material was obtained from the two whole soils, varied. With the clay soil, the total yield of light fraction organic-N was increased markedly by applying the densimetric technique to particle size components, rather than to the whole soil.Silt-size and fine clay-size particles from soils, sampled during rapid metabolism of microbial organic-[¹⁵N], were further fractionated densimetrically in “Nemagon”, sp. gr. 2.06. The organic-[¹⁵N] of the light and heavy subtractions changed markedly (P < 0.05) during periods of net ¹⁵N immobilization and mineralization, including a period after soil fumigation when extensive decomposition of [¹⁵N]-labelled microbial biomass occurred. Changes in the ¹⁵N of complementary light and heavy subfractions followed similar trends. Light subtraction organic-[¹⁵N] usually showed the greater relative change but the differences between the subtractions were not statistically significant. It is concluded that when small proportions only of soil organic-N are associated with macroorganic debris, as in these two soils amended wth glucose and ¹⁵NO^?₃, densimetric fractionation at a sp. gr. as high as 2.06 will yield light and heavy fractions, whose nitrogenous components are similarly available to biological attack. Enhanced metabolism of light fraction material is more likely to be demonstrated when such material consists mainly of obvious plant residues, and this may be more easily achieved by fractionation in liquids of sp. gr. <2.     

Corn yield variation as related to soil water fluctuation and nitrogen fertilizer. II. Soil water‐nitrogen‐yield relationships

Abstract

The aim of this study was to determine the relationships between soil water and nitrogen fertilizer and their effect on grain corn yield (Zea mays L.) in a zone where the limiting factor of yield and nitrogen efficiency is the water supply. The experiments were carried out for 10 years on a deep‐permeable well—drained chernozem in a temperate—continental dry climate with annual precipitation of about 500 mm.

Different nitrogen rates were applied and plant available soil water (PAW) was determined every year before and during the growing season. Multiple regressions were fitted for nitrogen rate, soil water and corn yield.

The results show that there is a significant interaction between soil water content, applied nitrogen and corn yield. The soil water explains the greatest part of yield variation, followed by the soil water‐added nitrogen interaction effect and the direct effect of added nitrogen. The PAH on July 1st gave a better correlation (R² = 0.88) than June 1st (R² = 0.85) or March 1st PAW (R² = 0.72). But the best correlation was obtained when both June and July PAW were taken together in the regression (R² = 0.914). July PAW was also more efficient in terms of yield per PAW. Thus, 1 mm of PAW on March, June and July 1st increased the control yield by 12.5, 14.6, and 18.3 kg grain/ha respectively, and by 18.0, 22.0 and 32.0 kg grain/ha for the fertilized yield (with 60 kg N/ha). At low soil moisture content, the applied N had no or even negative effect on water use efficiency and yield while at high PAW the water use efficiency was greatly increased by the applied N.     

Recent advances in the chemistry of nitrogen,phosphorus and potassium as fertilizers in soil: A review

The advent of civilization has made humans dependent on plants for food and medicine, leading to the intensification of agricultural production. The intense cultivation of crops has resulted in the depletion of available nutrients from soil, thereby demanding the application of excess nutrients to soil to improve yield. Thus, mineral fertilizer discovery and application have, in many ways, contributed greatly to meeting global food demands. However, aside from the positive effects of mineral fer...     

Relationships between four methods of organic carbon determination in leaves of nitrogen‐fixing trees and lignite‐based organic fertilizers

Abstract

Organic carbon (OC) in leaves of seven nitrogen (N₂)‐fixing trees and fifteen lignite‐based fertilizers was measured by loss‐on‐ignition (LOI at 500°C), wet oxidation by the Walkley‐Black method (CWB), Tinsley Dichromate Method (CTS), and dry combustion method using a LECO SC444 Carbon/ Sulphur Resistance Furnace Analyzer (CTO). There were significant differences in the capabilities of the methods in measuring OC from the organic materials with the quantity measured in the following order: LOI > CTO > CTS > CWB. A highly significant difference between LOI and CTO values suggested that components other than organic carbon (C) were removed by LOI since CTO gives total C value. The result also showed that N content in the organic materials was highly correlated with OC measured by individual methods. The LOI, CWB, and CTS were significantly correlated with CTO. The regression equations which were specific for either plant leaves or lignite‐based fertilizers indicated that any of the methods could be used to predict total C in the organic materials with a high degree of precision. In addition to the regression approach, an estimated correction factor of 1.4550 would be more appropriate to predict CTO from CWB for plant leaves than the 1.30 factor usually used for estimating oxidizable C in soils when CWB method is used. Also, a factor of 0.36180 could be used to estimate total C from LOI method for lignite fertilizers instead of merely regarding the difference in weight loss as the total organic matter.     

Ecological studies on coccoid bacteria in a pine forest soil—II. growth of bacteria introduced into soil

The growth of five typical but phenetically distinct cocci and Arthrobacter strains, isolated from a pine forest soil, has been investigated. Soil reaction was found to have a marked effect on growth and unless naturally acidic soils were made more alkaline they did not support growth, even in the presence of added nutrients. However, in the presence of fungi which could use the added nutrients, e.g. chitin, mycelial fragments etc., bacterial growth was possible and could be correlated with a decrease in acidity, especially around particles of organic matter. Where the pH rose above 7.9, bacterial growth again decreased. All the bacterial strains tested reacted in the same way, suggesting that they occupied similar microenvironments in both the acidic and alkaline soil horizons examined. Some explanations for the occurrence of nonsporing bacteria in soils in which apparently they cannot grow are suggested.     

Interactions of gamma‐irradiated sewage,nitrogen and phosphorus for Sorghum on a calcareous soil

Abstract

The interaction of gamma‐irradiated sewage sludge, nitrogen and phosphorus fertilizers on dry matter production, phosphorus concentration and phosphorus uptake of sorghum was examined. Three crops of sorghum were grown in the greenhouse in 19 1 plastic buckets. The phosphorus and sludge treatments were applied at the initiation of the experiment only. Nitrogen was applied to the corresponding nitrogen treatment pots before each of the three croppings.

There was a significant nitrogen x sewage interaction for dry matter production, phosphorus concentration and phosphorus uptake in each harvest. There was a significant phosphorus sewage sludge interaction in the first harvest for phosphorus uptake. All other possible interactions were not statistically significant. The 67 metric ton/ha sludge rate produced nearly the same yield as the nitrogen treatment. In the first harvest, sludge significantly increased plant phosphorus uptake from the fertilizer phosphorus. The phosphorus uptake in sorghum from 472 and 944 kg P/ha from the sludge treatments was comparable to that from 1299 and 2598 kg P/ha from triple superphosphate.     

Community level physiological profiles of microbial communities from forest humus polluted with different amounts of Zn,Pb, and Cd—Preliminary study with BIOLOG ecoplates

Abstract

Heavy metals may alter the structure and metabolic functions of soil microbial community. The objective of our study was to compare the community level physiological proffies (CLPPs) of microbial communities from forest humus polluted with different amounts of Zn, Pb, and Cd to test whether the addition of soluble Zn and Cd may affect the CLPPs of microbial communities. The samples were taken at 18 locations in southern Poland referred to as unpolluted (UP), slightly polluted (SP), and heavily polluted sites (HP). The contents of heavy metals were measured after wet digestions in concentrated HNO₃. Microbial communities were extracted using 0.96% NaCl solution. In order to test heavy metal tolerance of microbial communities from UP sites the extracts from these sites were additionally treated with Zn (50 mg L^-1; UP + Zn) and Cd (1 mg L^-1; UP + Cd). Metabolic functions of the microbial communities were analyzed using BIOLOG Ecoplates method. The contents of Zn, Pb and Cd were the highest at HP sites (4,740, 1,120, 41.0 mg kg^-1, respectively) followed by SP (830, 509, 9.2 mg kg^-1, respectively), and UP (173, 93, 2.1 mg kg^-1, respectively) sites. Principal components analysis (PCA) indicated that CLPPs at all sites were similar. This suggests that microbial community from SP and HP sites revealed tolerance to heavy metals. Addition of Zn affected CLPPs of microbial communities from UP sites as indicated by significantly (p < 0.05) higher value of PC1 score. The addition of Cd did not affect CLPPs of microbial communities from these sites.     

Interactions between Escherichia coli and allophane—I. Adsorption

Sorptive interactions between Escherichia coli (ATCC 11303B) and a purified allophane clay fraction were studied quantitatively using electronic particle counting and electrophoresis. Adsorption was influenced by pH and ions present at the allophane surface. These effects could be rationalized by considering changes in the net surface charge of the components. Electronic particle counting studies at pH 5.5 and above gave adsorption isotherms that obeyed single-term Langmuir kinetics. At pH 4.5, a more complex two-step isotherm was obtained, which was attributed to aggregation of unadsorbed cells by Al solubilized from the allophane surface.     

Europium chelate and fluorescent brightener staining of soil propagules and their photomicrographic counting—II. Efficiency

The efficiency of staining Lipomyces starkeyi and Pseudomonas aeruginosa cells added to agar and soil agar films and soil smears was examined using 2 mM europium(111) thenoyltrifluoroacetonate together with 25 μM disodium salt of 4,4'-bis (4-anilino-6-bis(2-hydroxyethyl) amino-S-triazin-2-ylamino) 2,2'-stilbene disulphonic acid. abbreviated to Eu(TTA)₃ and FB. respectively. The combined stains, or DFS (differential fluorescent stain), gave recoveries of added cells close to the expected values, but prestained cells lost their Eu(TTA)₃ fluorescence when added to agar at 55–60°C. Aqueous extracts of agar powder quenched the Eu(TTA)₃ fluorescence of cells, an effect which was attributed to water-soluble organic or inorganic ions in agar. It is suggested that the method of preparing soil-agar films and the long staining period required, effectively overcomes the quenching effect. Pre-stained cells were not affected by 10^?2 dilutions in soil.Photomicrographically recorded counts were not significantly different from visual counts made on the same fields.Comparative counts with phenol-aniline blue. fluorescein iso-thiocyanate and DFS showed the latter stain to be more efficient in differentiating soil propagules on and in soil organic matter.     

Response of wheat cultivars to different soil nitrogen and moisture regimes: II. Nitrogen up‐take,partitioning and influx 1

Nitrogen (N) is one of the major mineral nutrients required for growth and development of plants. Soil water availability, N concentration at the root surface and the ability of plants to absorb N are the most important factors that affect N uptake and partitioning. The objective of this study was to use greenhouse and growth chamber environments to investigate how two contrasting water regimes (stress and nonstress) and different soil N concentrations affect the uptake and distribution of N among different plant parts of three cultivars of wheat (Triticum aestivum L.) at different stages of development Results showed that at the beginning of stem elongation and under non N limiting conditions, there was a high and positive correlation between shoot dry matter production and shoot N content. Under N deficient soils that received different N rates, shoot N content was more related to shoot N concentration than to dry matter. Root growth and N content of the ‘Saada’ cultivar were negatively affected by high soil N concentration. Under mild water stress or nonstressed conditions, N uptake by the shoot increased with increased soil N in all cultivars. Overall, severe water stress masked the effect of N supply, and decreased N uptake in the case of ‘Merchouch 8’ and ‘Saada’. Root N content was not affected by water stress but increased when N was supplied. At anthesis and after rewatering plants from boot stage to anthesis, the plants fully recovered, and those that were water stressed, increased their N absorption to a rate much higher than those that were stressed. Nitrogen influx (NI) decreased with water stress, but increased more with increased soil N under well watered conditions than under stress. “Merchouch 8’ had higher NI than ‘Saada’. From this study we can conclude that the effect of N supply on N content was masked by severe water stress, and ‘Nesma’ was less sensitive to this stress. At anthesis, plants that were previously water stressed increased their rate of N uptake during the recovery. Root N was not affected by water stress but increased when soil N was increased.     

Studies of nitrogen immobilization and mineralization in calcareous soils—I: Distribution of immobilized nitrogen amongst soil fractions of different particle size and density

¹⁵NO₃^? was immobilized in a calcareous clay and a calcareous sandy soil during incubation of each soil with glucose and wheat straw. Changes in the distribution of immobilized ¹⁵N amongst soil extracts and soil fractions of different particle size and density were determined during periods of net N immobilization.The nature of the organic-C amendment, but not soil type, significantly influenced both the distribution of the immobilized ¹⁵N and the pattern of changes of the organic-¹⁵N of soil fractions with time. In straw-amended soils, approx. 20% of the organic-¹⁵N became associated with a light fraction, sp. gr. < 1.59, the remainder becoming distributed mainly amongst the silt and clay fractions. In glucoseamended soils, very little (< 1.2%) of the ¹⁵N was immobilized in the light fraction, sp. gr. < 1.59, most being rapidly distributed amongst the silt and clay fractions. During a period of complete immobilization, organic-¹⁵N was transferred from the fine clay to the silt and coarse clay fractions.Silt, coarse clay and fine clay components from glucose-amended soils sampled at the end of the net immobilization phase were further fractionated densimetrically into light (sp. gr. < 2.06) and heavy (sp. gr. > 2.06) subfractions. The organic-¹⁵N of respective light subfractions accounted for 43–64% of the total organic-¹⁵N of the silt, 1–9% of that of the coarse clay and 19–21% of that of the fine clay fractions.     

Reducing nitrogen leaching‐losses from containerized plants: The effectiveness of controlled‐release fertilizers

Abstract

To evaluate the effectiveness of controlled‐release fertilizer (CRF) for reducing nitrogen (N) leaching‐losses from containerized greenhouse crops, three experiments were conducted where CRFs were applied in different ways and compared to water‐soluble fertilizer (WSF). In each experiment, ‘First Lady’ marigold (Tagetes erecta L.) plants in 0.5‐liter pots of a soilless growth medium were fertilized with the same amount of ? from 20N‐4.3P‐16.6K WSF, Osmocote 14N‐6.2P‐11.6K CRF, or Nutricote 14N‐6.2P‐11.6K CRF fertilizers. The volume of irrigation water applied to all treatments was the same in each experiment. Nitrogen content, as NH₄‐N and NO₃‐N in container leachates, and plant growth were measured and used to compare WSF with CRFs incorporated in the growth medium, or as applied to the surface, in either one large application or two small doses. A single large application of CRF at planting resulted in as much or more ? leaching than the regular application of WSF. Effectiveness of CRFs in limiting ? leaching was greatly increased by making two smaller applications, the first at planting and the second 15 to 35 days later. More ? was recovered in the leachate when CRFs were incorporated in the growth medium compared to surface application. Regardless of fertilizer type, application method, timing of application, or for each individual experiment, NO₃‐N was the predominant ? form found in the leachate and more than one‐half of the total amount of ? leached during each experiment was recovered within 30 days of planting.