Effects of nitrapyrin,terrazole, and simazine on soil nitrogen transformation and corn growth

Abstract

Nitrapyrin, terrazole and simazine were evaluated as chemical inhibitors of biological nitrification and denitrification. Corn (Zea mays L. cv. Hybrid Pioneer 3343) was grown in 60‐liter pots filled with a 50/50 (V/V) sand/Cecil clay mixture. Chemical treatments consisted of weekly applications of 0.25 ppm nitrapyrin, terrazole and/or simazine concurrently with 20 ppm N as either (NH₄)₂SO₄ or Ca(NO₃)₂ for 9 weeks. Thereafter, only N (20 ppm per pot) was applied to the media every three days for 4 weeks. Nitrapyrin, terrazole and simazine reduced nitrification resulting in both higher total plant N and residual soil NH₄ content relative to the control plants and soil. Plant growth was reduced by the inhibitory effects of the chemicals on nitrification and subsequent NH₄ accumulation in the medium. All chemicals reduced denitrification with terrazole being more effective than nitrapyrin as reflected by higher N contents of plants and residual soil NO₃‐N. Nitrapyrin and/or terrazole applied with Ca(NO₃)₂ increased plant biomass, but simazine, by inducing higher N0₂ concentration in the plant tissues, sharply reduced plant growth relative to the other treatments. When simazine was part of the chemical treatment, its effects on plant growth and total N contents generally outweighed or masked those of nitrapyrin or terrazole.     

Short‐term effects of polyacrylamide and dicyandiamide on C and N mineralization in a sandy loam soil

The soil conditioners anionic polyacrylamide (PAM) and dicyandiamide (DCD) are frequently applied to soils to reduce soil erosion and nitrogen loss, respectively. A 27‐day incubation study was set up to gauge their interactive effects on the microbial biomass, carbon (C) mineralization and nitrification activity of a sandy loam soil in the presence or absence of maize straw. PAM‐amended soils received 308 or 615 mg PAM/kg. Nitrogen (N)‐fertilized soils were amended with 1800 mg/kg ammonium sulphate [(NH₄)₂SO₄], with or without 70 mg DCD/kg. Maize straw was added to soil at the rate of 4500 mg/kg. Maize straw application increased soil microbial biomass and respiration. PAM stimulated nitrification and C mineralization, as evidenced by significant increases in extractable nitrate and evolved carbon dioxide (CO₂) concentrations. This is likely to have been effected by the PAM improving microbial conditions and partially being utilized as a substrate, with the latter being indicated by a PAM‐induced significant increase in the metabolic quotient. PAM did not reduce the microbial biomass except in one treatment at the highest application rate. Ammonium sulphate stimulated nitrification and reduced microbial biomass; the resultant acidification of the former is likely to have caused these effects. N fertilizer application may also have induced short‐term C‐limitation in the soil with impacts on microbial growth and respiration. The nitrification inhibitor DCD reduced the negative impacts on microbial biomass of (NH₄)₂SO₄ and proved to be an effective soil amendment to reduce nitrification under conditions where mineralization was increased by addition of PAM.     

Variation in the relationship between nitrification and acidification of subtropical soils as affected by the addition of urea or ammonium sulfate

The effects on nitrification and acidification in three subtropical soils to which (NH₄)₂SO₄ or urea had been added at rate of 250 mg N kg⁻¹ was studied using laboratory-based incubations. The results indicated that NH₄⁺ input did not stimulate nitrification in a red forest soil, nor was there any soil acidification. Unlike red forest soil, (NH₄)₂SO₄ enhanced nitrification of an upland soil, whilst urea was more effective in stimulating nitrification, and here the soil was slightly acidified. For another upland soil, NH₄⁺ input greatly enhanced nitrification and as a result, this soil was significantly acidified. We conclude that the effects of NH₄⁺ addition on nitrification and acidification in cultivated soils would be quite different from in forest soils. During the incubation, N isotope fractionation was closely related to the nitrifying capacity of the soils.     

Nitrapyrin,terrazole, atrazine,and simazine influence on nitrification and corn growth

Most farming systems involving tilled crops require use of pesticides and nitrogen fertilizers in different combinations although most pesticides effects on soil N transformation are scantly documented. Studies were initiated to compare atrazine and simazine herbicides with two biological nitrification inhibitors (nitrapyrin and terrazole) for their effects on biological nitrification and corn (Zea mays L.) growth. In a laboratory study, inhibition of nitrification was less than 3% in a Tifton loamy sand incubated with 10 μg a.i g^‐1 soil atrazine or simazine but was more than 10% in soil amended with nitrapyrin or terrazole, applied separately or in combinations with either herbicide at the same rate. Similar trends were observed with soil treated with different combinations of 2.5 μg a.i. g^‐1 soil nitrapyrin or terrazole and 1.25 μg a.i. g^‐1 soil atrazine or simazine and incubated with and without corn plants under greenhouse conditions. The combination of either herbicide with nitrapyrin or terrazole significantly reduced the corn dry weights with substantial accumulation of Kjeldahl N and NO₃ ^‐ in tissues of plants, probably due to a concentration effect. However, these chemical combinations, applied at the rate of 1.2 kg a.i. ha^‐1 in conjunction with 35 kg ha^‐1 N as (NH₄)₂SO₄ in split banded applications (at planting and at the 6^th leaf stage), showed a nonsignificant trend towards increased corn ear yields in two‐year field studies. Generally, when atrazine or simazine was part of the chemical treatment, its effects on nitrification, plant growth and total N contents outweighed or masked those of nitrapyrin or terrazole.     

Effect of high ammonium levels on nitrification,soil acidification,and exchangeable cation dynamics

Abstract

In almond orchards which are fertilized and irrigated with drip systems, fertilizers are applied to a relatively small soil volumes several times during the growing season. Where NH₄‐based fertilizers are used, high NH₄ levels are anticipated in soil solution and on exchange sites. The effects of high NH₄ concentration on nitrification, soil acidification, and exchangeable cation dynamics were studied in an incubation experiment where 500 and 2000 mg N/kg soil were added as (NrL₄)₂SO₄. After incubation for 25 days with added (NH₄)₂SO₄, nitrifying bacteria were lower than the populations at the start of experiment. In the 2000 mg N/kg treatment, nitrification activity nearly ceased and soil acidification was reduced. Although nitrification activity was lower in the 500 mg N/kg treatment than in the control, after 10 days of incubation, nitrification activity lowered soil pH by 0.7 units. After the initial 10 days, soil pH was lowered to 4.8 and nitrification activity was depressed. Ammonium ions occupied about 20 and 36 % of the exchange capacity in the 500 and 2000 mg N/kg treatments respectively, and exchangeable Ca, Mg, and K were significantly lowered. Extractable acidity was less than 0.1 cmoiykg dry soil.     

Nitrification in soils incubated with pig slurry

Incubation studies (5 weeks at 30°C) of nitrification were made in an acid (pH 5.8) and a neutral (pH 7.1) soil receiving varying concentrations of pig slurry and (NH₄)₂SO₄ solution. Mineral-N and pH changes were observed at weekly intervals and inorganic salts media were used to obtain separate estimates of the numbers of NH₄-N- and NO₂-N-oxidizing bacteria. In the acid soil, pig slurry NH₄-N was nitrified to a greater extent than (NH₄)₂SO₄. In the neutral soil, slurry additions resulted in the accumulation of NO₂^?-N and, in one case, the complete inhibition of nitrification for 4 weeks. Slurry raised the pH of both soils more than (NH₄)₂SO₄ and nitrification in the acid soil was most rapid in a 2 week period of elevated pH following slurry applications. Numbers of Nitroxomonas isolated from the acid soil were considered high enough to account for NH₄-N oxidation in slurry-treated samples. Numbers of nitrifiers recovered from the incubated neutral soil samples were variable but frequently high enough (>10⁴/g dry soil) to account for observed rates of nitrification. Results are discussed in relation to heterotrophic nitrification in soils, and the practical implications of spreading slurry on agricultural land.     

Transformations of nitrogen fertilizers in soil

The effects of ¹⁵N-labelled urea, (NH₄)₂SO₄ and KNO₃ on immobilization, mineralization, nitrification and ammonium fixation were examined under aerobic conditions in an acid tropical soil (pH 4.0) and in a neutral temperate soil (pH 6.8). Urea, (NH₄)₂SO₄ and KNO₃ slightly increased net mineralization of soil organic nitrogen in both soils. There was also an apparent Added Nitrogen Interaction (ANI) i.e. added labelled NH₄-N stood proxy for unlabelled NH₄-N that would otherwise have been immobilized. So far as immobilization and nitrification were concerned, urea and (NH₄)₂SO₄ behaved very similarly in each soil. Immobilization of NO₃-N was negligible in both soils. Some of the added labelled NH₄-N was rapidly fixed, more by the temperate soil than by the tropical soil. This labelled fixed NH₄-N decreased during incubation, in contrast to labelled organic N, which did not decline.     

Effect of dicyandiamide on the form and recovery of 15N‐labeled urea in the delayed flood soil system

Abstract

Dicyandiamide (DCD) is a nitrification inhibitor that has been proposed for use in drill‐seeded rice. Immobilization of fertilizer NH₄ ⁺‐N by soil microorganisms under aerobic conditions has been found to be significantly enhanced in the presence of a nitrification inhibitor. The objective of this laboratory study was to determine if DCD significantly delayed nitrification of urea‐derived N, and if this enhanced immobilization of the fertilizer N in the delayed‐flood soil system inherent to dry‐seeded rice culture. Nitrogen‐15‐labeled urea solution, with and without DCD (1: 9 w/w N basis), was applied to a Crowley silt loam (Typic Albaqualf) and the soil was incubated for 10 weeks in the laboratory. The soil was maintained under nonflooded conditions for the first four weeks and then a flood was applied and maintained for the remaining six weeks of incubation. The use of DCD significantly slowed the nitrification of the fertilizer N during the four weeks of nonflooded incubation to cause the (urea + DCD)‐amended soil to have a 2.5 times higher fertilizer‐derived exchangeable NH₄+‐N concentration by the end of the fourth week. However, the higher exchangeable NH₄+‐N concentration had no significant effect on the amount of fertilizer N immobilized during this period. Immobilization of the fertilizer N appeared to level off during the nonflood period about the second week after application. After flooding, immobilization of fertilizer N resumed and was much greater in the (urea + DCD)‐amended soil that had the much higher fertilizer‐derived exchangeable NH₄ ⁺‐N concentration. Immobilization of fertilizer N appeared to obtain a maximum in the urea‐amended soil (18%) about two weeks after flooding and for the (urea + DCD)‐amended soil (28%) about four weeks after flooding.     

Transformations and recovery of residue and fertilizer nitrogen-15 in a sandy Lixisol of West Africa

 The fate of ¹⁵N-labeled plant residues from different cover-cropping systems and labeled inorganic N fertilizer in the organic, soil mineral, microbial biomass and soil organic matter (SOM) particle-size fractions was investigated in a sandy Lixisol. Plant residues were from mucuna (legume), lablab (legume), imperata (grass), maize (cereal) and mixtures of mucuna or lablab with imperata or maize, applied as a surface mulch. Inorganic N fertilizer was applied as ¹⁵N-(NH₄)₂SO₄ at two rates (21 and 42 mg N kg^–1 soil). Total N release from mucuna or lablab residues was 2–3 times higher than from the other residues, whereas imperata immobilized N throughout the study period. In contrast, ¹⁵N was mineralized from all the plant residues irrespective of the mineralization–immobilization pattern observed for total N. After 168 days, 69% of soil mineral N in mucuna- or lablab-mulched soils was derived from the added residues, representing 4–8% of residue N, whereas 9–30% of inorganic N was derived from imperata, maize and the mixed residues. At the end of the study, 4–19% of microbial biomass N was derived from the added residue/fertilizer-N, accounting for 1–3% of added residue-N. Averaged across treatments, particulate SOM fractions accounted for less than 1% of the total soil by weight but contained 20% of total soil C and 8% of soil N. Soils amended with mucuna or lablab incorporated more N in the 250–2000 μm SOM pool, whereas soil amended with imperata or the mixed residues incorporated similar proportions of labeled N in the 250–2000 μm and 53–250 μm fractions. In contrast, in soils receiving the maize or inorganic fertilizer-N treatments, higher proportions of labeled N were incorporated into the 53–250 μm than the 250–2000 μm fractions. The relationship between these differences in residue/fertilizer-N partitioning into different SOM particle-size fractions and soil productivity is discussed. Received: 12 March 1999     

Transformation of urea and ammonium nitrate in an entisol and a spodosol under citrus production

Abstract

Chemical transformations of ammonium nitrate (NH₄NO₃) and urea‐nitrogen (N), at different rates of application, were studied in a Candler (Typic Quartzipsamment) and Wabasso (sandy, Alfic Haplaquod) sand by incubating fertilized surface soil (from 0 to 15 cm depth) samples at 10% moisture content (by weight) in the laboratory at 25±1°C. During the 7 d incubation, the percentage of transformation of NH₄‐N into NO₃‐N was 33 to 41 and 37 to 41% in the Candler fine sand and Wabasso sand, respectively, at application rates of 1.00 g N kg¹. In a parallel experiment, 85 to 96% of urea applied (equivalent to 0.25 to 1.00 g N kg^‐1soil) was hydrolyzed to NH₄‐N within 4 d in the Candler soil, whereas it required 7 d to hydrolyze 90 to 95% of the urea applied in the Wabasso soil. No nitrification was evident for 30 days in the Candler fine sand which received urea application equivalent to ≥ 0.50 g N kg^‐1. In the urea‐amended Wabasso sand, the formation of NO₃ decreased as the rate of urea‐N increased. Possible loss of N from NH₃ volatilization or inhibition of activity of nitrifiers due to elevated soil pH (8.7 to 9.2) during the incubation of urea amended soils may have caused very low nitrification.     

Symbiosis of Trifolium subterraneum with mycorrhizal fungi and Rhizobium trifolii as affected by ammonium sulphate and nitrification inhibitors

The symbioses between Trifolium subterraneum, mycorrhizal fungi and Rhizohium are affected by (NH₄)₂SO₄ and by the nitrification inhibitors 2-chloro-6 (trichloromethyl) pyridine (N-Serve) and 2-trichloromethyl pyridine (2TMP). At 50 μg · g^?1 soil N-Serve and 2TMP had toxic effects on plant growth, measured as leaf expansion, root length and dry weight. Lower concentrations of N-Serve also produced some toxic symptoms. The addition of (NH₄)₂SO₄ to the soil at 2 and 6 m-equiv NH⁺₄ per pot, resulted in reduced root length and nodulation. Shoot dry weight was reduced at 6 m-equiv NH⁺₄ per pot. In the presence of (NH₄)₂SO₄ the toxic effects of the nitrification inhibitors on plant growth were less.Both nitrification inhibitors reduced development of mycorrhizal entry-points and extent of root colonization (% infection). Percentage infection of the root system was also reduced by (NH₄)₂SO₄. Development of nodules on the lateral roots was increased in the presence of N-Serve at 5 and 15 μ · g^?1. This effect, however, was accompanied by a marked reduction in N₂ase activity. Smaller increases in nodulation were apparent with 2TMP and were associated with variable N₂ase activity.     

Methane oxidation in arable soil as inhibited by ammonium, nitrite, and organic manure with respect to soil pH

 The effects of inorganic N and organic manure, applied to a loamy arable soil, on CH₄ oxidation were investigated in laboratory incubation experiments. Applications (40 mg N kg^–1) of NH₄Cl, (NH₄)₂SO₄, and urea caused strong instantaneous inhibition of CH₄ oxidation by 96%, 80%, and 84%, respectively. After nitrification of the added N the inhibitory effect was not fully reversible, resulting in an residual inhibition of 21%, 16%, and 25% in the NH₄Cl, (NH₄)₂SO₄, and urea treatments, respectively. With large NH₄ ⁺ applications [240 mg N kg^–1 as (NH₄)₂SO₄] the residual inhibition was as high as 64%. Exogenous NO₂ ^– (40 mg NO₂ ^–-N kg^–1) initially inhibited CH₄ oxidation by 84%, decreasing to 41% after its oxidation. Therefore, applied NO₂ ^– was a more effective inhibitor of CH₄ consumption than NH₄ ⁺. Temporary accumulation of NO₂ ^– during nitrification of added N was small (maximum: 1.9 mg NO₂ ^–-N kg^–1) and thus of minor importance with respect to the persistent inhibition after NH₄ ⁺ or urea application. CH₄ oxidation after NaNO₃ (40 mg N kg^–1) and NaCl addition did not differ to that of the untreated soil. The effect of organic manures on CH₄ oxidation depended on their C/N ratio: fresh sugar beet leaves enhanced mineralization, which caused an instantaneous 20% inhibition, whereas after wheat straw application available soil N was rapidly immobilized and no effect on CH₄ oxidation was found. The 28% increase in CH₄ oxidation after biowaste compost application was not related to its C/N ratio and was probably the result of an inoculation with methanotrophic bacteria. Only with high NH₄ ⁺ application rates (240 mg N kg^–1) could the persistent inhibitory effect partly be attributed to a pH decrease during nitrification. The exact reason for the observed persistent inhibition after a single, moderate NH₄ ⁺ or urea application is still unknown and merits further study. Received: 31 October 1997     

Greenhouse Gas Emissions from Paddy Soils Respond to Different Crop Root Residues and N Fertilizer Types

Greenhouse gas emissions from paddy soils respond differently to different combinations of crop root residues and N forms. An incubation experiment was carried out to explore the effect of four crop residues (milk vetch, ryegrass, winter wheat, and rape) and four nitrogen treatments (without fertilizer, urea, (NH₄)₂SO₄, and KNO₃) on CH₄, CO₂, and N₂O emissions in a paddy soil. Except in KNO₃ application treatments, CH₄ emissions of milk vetch residue treatments were significantly higher than those of the rest residue treatments. In the presence of milk vetch and ryegrass residues, urea application significantly increased CH₄ emissions in comparison to treatments without fertilizer. Urea significantly promoted CO₂ emissions, whereas (NH₄)₂SO₄ and KNO₃ significantly inhibited CO₂ emissions at all root residue treatments. Urea did not increase N₂O emissions, but (NH₄)₂SO₄ and KNO₃ promoted N₂O emissions at all residue treatments. In addition, KNO₃ had more effects on the increase of N₂O emissions than (NH₄)₂SO₄ in milk vetch-amended soils. Urea addition had no effect on global warming potentials, and (NH₄)₂SO₄ and KNO₃ addition significantly increased global warming potentials at all residue treatments except KNO₃ + winter wheat residue combination. Our results indicated that urea application had no additive effect on global warming when root residues were left in paddy soils, whereas (NH₄)₂SO₄ and KNO₃ application could increase the risk of global warming.     

Correction of iron chlorosis in peanut (arachis hypogea shulamit) by ammonium sulfate and nitrification inhibitor

Peanut (Arachis hypogea cv. Shulamit) grown on very high calcium carbonate (CaCO₃) content soils is showing iron (Fe) chlorosis symptoms. Supplying the plant with ammonium sulphate ((NH₄)₂SO₄) in the presence of nitrapyrin (N‐Serv) for preventing nitrification reduced Fe chlorosis. Nitrate (NO^‐ ₃) developed in the soil with time, even with nitrapyrin present. When ammonium (NH⁺ ₄) was even less than 20% of the total mineral N in the soil, no Fe‐stress could be observed, suggesting that the NH⁺ ₄ uptake by the plant and the consequence of hydrogen (H⁺) efflux occurs from the root to the rhizosphere, resulting in a decrease of redox potential near the root, and solubilizing enough Fe near the root to overcome the chlorosis.     

Decomposition rate of dicyandiamide and nitrification inhibition

Abstract

Degradation of dicyandiamide (DCD) was assayed in laboratory studies at 8, 15, and 22 C in a Decatur silt loam and in a Norfolk loamy sand. Dicyandiamide was very short lived at 22 C, with half‐lives of 7.4 and 14.7 days in the Decatur and Norfolk soils, respectively. In the Norfolk soil at 8 C, half‐life increased to 52.2 days. In a nitrificaton study of both soils at 22 C, 80 mg (NH₄)₂SO₄‐N kg^‐1 of soil was applied with 20 mg DCD‐N kg^‐1 of soil and 100 mg kg^‐1 (NH₄)₂S0₄‐N was added with 5% nitrapyrin. Distinct lag phases preceded zero order nitrification with the inhibitor treatments. Lag periods were 2 and 2.6 times the half life of DCD in the degradation study for Decatur and Norfolk soils, respectively. Like most nitrification inhibitors, the effectiveness of DCD decreases with increasing temperature. In the Norfolk loamy sand, nitrification inhibition by DCD was equal to nitrapyrin for up to 42 days, but in Decatur silt loam, DCD was less potent to nitrapyrin as a nitrification inhibitor.     

Nitrogen transformations of ammonium sulfate and alanine in submerged Maahas clay

The fate of added nitrogen in submerged soils was studied using ¹⁵N-labelled ammonium sulfate and alanine. After 8 weeks of incubation 25 and 22%, respectively, of nitrogen from ammonium sulfate and alanine were recovered in the soil. Under the experimental conditions used nitrogen added to presubmerged soils was lost rapidly outside of the soil-water system, regardless of whether the nitrogen was organic or inorganic. Fractionation studies revealed that the amount of tagged N incorporated into exchangeable ammonium, residual fractions, volatilized as NH₃ and chemically fixed nitrogen was not enough to account for the nitrogen loss. The nitrogen loss was attributed to nitrification and subsequent denitrification during the incubation period.

The effect of N-Serve [2-chloro-6-(trichloromethyl)pyrimidine] on nitrification of ¹⁵N-labelled (NH₄)₂SO₄-in submerged soils was studied. About 15% more nitrogen was recovered from non-presubmerged soils, and less nitrate was accumulated in presubmerged soils where N-Serve coated (NH₄)₂SO₄ was applied, than from soils where (NH₄)₂SO₄ was applied without N-Serve. Presubmerged soils provided a more favorable environment for nitrification than for denitrification under the experimental conditions used.     

Umsetzung 14C-markierter Pflanzeninhaltsstoffe im Boden in Gegenwart von 15N-Ammonium

Turnover of ¹⁴C-labelled plant components and ¹⁵N-ammonium in soil The turnover of ¹⁴C-labelled glucose, cellulose, wheat straw, phenols or of lignin in soil was investigated in the presence of (¹⁵NH₄)₂SO₄. The plant components were more or less rapidly degraded to ¹⁴CO₂ and the amended nitrogen source became organically linked but was also remineralized to a variable extend. Also variable was the incorporation of the ¹⁴C or ¹⁵N into humified residues or microbial metabolites. During the turnover of carbohydrates and straw a rapid increase of ¹⁴C and ¹⁵N in amino-acids or unidentified components of soil hydrolysates occurred which was followed by a decrease. The turnover of phenols was mostly similar to that of carbohydrates but compared to their mineralization rates, a smaller incorporation occurred into the easily hydrolyzable soil fractions. Although lignin was considerably mineralized to CO₂, the incorporation of the carbon remaining in soil into hydrolyzable components especially in amino-acids was, however, very small. A somewhat higher amount became incorporated into unidentified components of hydrolysates, but the bulk of the lignin carbon remained in the non-hydrolizable residue.     

Sources of spatial and temporal variability of inorganic nitrogen in pure and mixed deciduous temperate forests

We investigated the influence of tree canopy composition and structure on the spatial and temporal variability of (i) concentrations of inorganic N (NH₄⁺ and NO₃⁻) and (ii) net N-mineralization and net nitrification, within the temperate forest floor. We compared a pure European beech stand (PS) with a mixed beech-hornbeam one (MS). Three sampling areas were chosen in each stand. Within the PS, the tree locations represented a decreasing gradient of light intensity reaching the forest floor. Within the MS they represented a gradient in the amount of hornbeam leaves present in the litter. In the field NH₄⁺ and NO₃⁻ concentrations were measured in the upper mineral soil (UMS) and the overlying organic layers (OL and OF+OH). Field exposures using buried bags were carried out on UMS over 1 year to measure in situ net N-mineralization and net nitrification. Potential net N-mineralization and net nitrification were investigated in summer with UMS, OL and OF+OH incubated at 28 °C for 28 days in the laboratory. We hypothesize that with the presence of a mull-forming species (hornbeam) within a stand dominated by a moder-forming one (European beech), (i) the spatial and (ii) temporal patterns of soil inorganic N concentrations, net N-mineralization and net nitrification would be different in the two stands. Our main results show that tree species composition has an influence on both spatial and temporal patterns of nitrification. The PS exhibited its highest peaks of UMS NO₃⁻ concentration and net nitrification in spring and early summer while they were highest in the MS in winter. Furthermore, PS exhibited a higher rate of net nitrification than MS. We discuss this unexpected result and suggest that dissolved organic C may be the controlling factor for net nitrification in the MS.     

Acidification in the Rhizosphere of Rape Seedlings and in Bulk Soil by Nitrification and Ammonium Uptake

Ammonium salts used as fertilizers may cause soil acidification by two different processes: nitrification in soil and net release of protons from roots. Their influence on soil pH may vary depending on the distance from root surface. The aim of this study was to distinguish between these two processes. For this purpose rape seedlings were grown 10 d in a system which separated roots from soil by a fine-meshed screen. As a function of distance from the plane root layer formed on the screen, pH, titratable and exchangeable acidity and NO₃- and NH₄-nitrogen were determined. The soil, a luvisol from loess, was supplied with no N or (NH₄)₂SO₄ either with or without a nitrification inhibitor (DCD). The bulk soil pH remained unaffected when no N or 400 mg NH₄? N kg^?1 soil plus DCD was applied but it decreased from 6.6 to 5.8 without DCD. In contrast, rhizosphere pH decreased in all cases, mainly within a distance of 1 mm from the root plane only, but with gradients extending to between 2 and 4 mm into the soil. The strongest pH decrease, from 6.6 to 4.9, occurred at the root surface of plants treated with both NH₄-N and DCD where most of the mineral N remained as ammonium. In this case Al was solubilized in the rhizosphere as indicated by exchangeable acidity. Total soil acidity produced in the NH₄ treatment without DCD was mainly derived from nitrification compared to root released protons. However, acidification of the rhizosphere was diminished by nitrification because nitrate ions taken up by the roots counteracted net proton release. It is concluded that nitrification inhibitors may reduce proton input from ammonium fertilizers but enhance acidification at the soil-root interface which may cause Al toxicity to plants.     

Simultaneous nitrification and diffusion in soil. III. The effects of the addition of ammonium sulphate

The simultaneous nitrification and diffusion of NH₄⁺, applied as ammonium sulphate to laboratory columns, was followed experimentally and with a simulation model. Ammonium was applied as a fertilizer band at levels equivalent to 69 kg N ha^?1 to a 1 cm depth. The concentration profiles of NH₄⁺, NO₃^?, SO^2?₄ and pH were measured in two columns for incubation times of 214 and 286 h. The simulation model provided for the precipitation and ion pair formation of CaSO₄, the adsorption equilibria of NH₄⁺ and soil acid with the soil solid phase, and nitrifier growth and activity. In general, good agreement was found between the experimental and simulated concentration profiles. The effect of CaSO₄ precipitation on the diffusion of N was investigated using model simulations of the diffusion of NH₄⁺ in the absence of nitrification. The simulations suggested that the reactions of SO^2?4 in the soil could markedly affect the spread of NH₄⁺ from a band of (NH₄)₂SO₄.