Fixed ammonium in Libyan soils and its availability to barley seedlings

Summary Native fixed ammonium nitrogen and fixation of added ammonium nitrogen were studied in soil profile samples of three Libyan soils. The availability of both forms of fixed ammonium N to barley seedlings was investigated using surface soil samples under pot culture.All soils contained native fixed ammonium N which ranged from 9.26 to 10.36 mg/100 g soil. Fixation of added ammonium N was of the order of 5.10 mg/100 g for surface soils and 5.26 mg/100g for sub-surface soils. Fixation increased with profile depth.It was found that 38 percent of the soil total fixed ammonium N and 70 percent of the soil KOBr extractable N were available to barley seedlings. An equation representing the uptake of N from these two sources was established and their contribution to plant content of N was calculated.     

Ammonium fixation by some soils in the ussr and the availability of this ion to plants

Summary The ability of various soils to fix ammonium in unexchangeable form was studied. Soils in their natural state contain unexchangeably fixed NH₄. The amount of which considerably increases with systematic fertilization and in soils with high nutrient status, but the ability of these soils for extra fixation of ammonium decreases. Chernozem soils are able to fix ammonium in unexchangeable form in considerably greater quantities than soddy-podzolic soils. All soils show a little increase of ability to fix ammonium with profile depth. The heavier is the soil the greater is its ability for fixation of NH₄ in unexchangeable form.In the conditions of a greenhouse experiment unexchangeably fixed NH₄ was used by plants very poorly. Exchangeably absorbed ammonium is available to plants, although to a lesser extent than water soluble salts. Soils fix ammonium to a greater amount from NH₄OH than from ammonium nitrate, hence the latter is a better source of nitrogen for plants than ammonia liquor solution if applied to soils with a definite abolity to fix unexchangeable ammonium.     

Effectiveness of some iron phosphates as sources of phosphorus for plants

Summary Two well-characterized crystalline ferric phosphates, two colloidal ferric phosphates, and fluorapatite were tested under greenhouse conditions as sources of phosphorus for corn over a 3-cropping period. The selected compounds are representative of those expected to form in soils as reaction products from more soluble phosphate fertilizers.Strengite, FePO₄·2H₂O, was completely unavailable in acid soils and gave only a slight phosphorus response on soils limed to pH 7.6. Uptake of P from hydrogen ammonium ferric phosphate, H₈NH₄Fe₃(PO₄)₈·6H₂O, was approximately 70 per cent that from MCP, and increased with cropping.The colloidal ferric phosphates were approximately 78 per cent as available as MCP and became more available with liming and cropping. In the soil limed to pH 6.5, their effectiveness increased from 47 per cent that of MCP in the first crop to 100 per cent as effective by the third crop.Fluorapatite, included as an insoluble calcium phosphate source, was completely unavailable.     

Methods of measuring available nutrients in West Indian soils

Summary Total K, exchangeable K (NH₄OAc method), CH₃COOH, cold H₂SO₄ and boiling HNO₃ extractable K were compared with dry matter yield response and K uptake from maize grown on 155 Commonwealth Caribbean soils in greenhouse experiments.Correlation coefficients for soil test values with percentage yield and K uptake were calculated using data from all the soils together and also when the soils were grouped according to pH (< 5.5, 5.5–7.0 and > 7.0), per cent base saturation (< 60, 60–79, 80–99 and 100 per cent), cation exchange capacity (< 10, 10–30 and > 30 me per 100 g) and texture (clays, clay loams and loams and sands). In general, correlations of soil test value with K uptake were superior to those with percentage yield. Total K gave no significant correlations in any of the comparisons. The NH₄OAc (exchangeable K) and cold H₂SO₄ were the most successful methods overall and the least sensitive to changes in soil properties. The CH₃COOH extract in general was the least effective. The differing behaviour and the ability of the methods to extract K is discussed in relation to the mineralogy and genesis of the soils which make up the various groups when divided according to the soil properties listed above.     

Studies on potassium release in an inceptisol soil (Holambi Series) at the minimum level of exchangeable potassium

Summary Ammonium acetate extractable potassium in the soil reached a minimum value of 6.8 mg K/100g soil after 14 crops of wheat and pearl millet in the field without applying any potassium fertilizer. At this level of ammonium acetate extractable K both wheat and pearl millet utilized about, 90 per cent of the total K from non-exchangeable sources. Wheat and pearl millet were grown in this soil in the greenhouse at different levels of K. At K₀ level wheat utilized 86 per cent of the total K uptake from the non-exchangeable source and pearl millet, 95 per cent. At K₁ level, wheat utilized only 19 per cent but at higher levels of K, there was build up in the K status of soils. In the case of pearl millet at K₁, K₂ and K₃ levels 59, 13 and 22 per cent of total uptake were contributed by non-exchangeable forms. The total K uptake by pearl millet was more than double that by wheat. Plant analysis showed that 83 per cent of the total K in wheat was contained in the shoot portion and the rest in the roots. The corresponding figures for pearl millet were 94 and 6 per cent.     

Fixation and release of potassium and ammonium ions in Danish soils

Summary Results of a laboratory investigation showed that among soils in Denmark it are chiefly those rich in clay minerals that will fix and release potassium and ammonium. The two cations were fixed in nearly equivalent proportions, but ammonium was fixed preferentially to potassium when added together to the soil. The maximum fixation reached 20 to 30 per cent of the addition in top soil layer but 50 to 80 in subsoil. Soils from a permanent fertilizer experiment showed the strongest fixation and least release of potassium where no potassic fertilizer had been applied for more than 70 years. In soils from another field experiment on residual effect of various nitrogenous fertilizers there was a small but significant increase in content of inorganically fixed ammonium where urea had been applied.     

Tracer studies on the balance and chemical distribution of applied nitrogen under different moisture regimes using lysimeter

Summary Tracer studies were made on balance and chemical distribution of added fertilizer under field conditions using a modified type of lysimeter at different moisture regimes. A modified chemical method was also used for the determination of different forms of organic N.An average of 25 per cent of the isotope enriched nitrogen applied to soil could not be accounted for at the end of the 3 years of experiment. The amount of residual added N in soil was around 33 per cent of which 27 per cent was in 0–20 cm layers and only 6 per cent was found in 20–50 cm layers. The average crop recoveries were around 43 per cent. Only 0.18 per cent of NO₃–N was leached from the irrigated plots.The alkali-stable N (amino acid-N) fraction was higher for irrigated (19 per cent) than nonirrigated plots (15 per cent). There were no difference in the amounts of fixed NH₄, non-hydrolyzed and alkali-labile N fractions for irrigated and non-irrigated plots. Only an average of 1.5 per cent of total fertilizer N was found as fixed NH₄–N form but the total fixed NH₄–N was higher (10–13 per cent) than that reported by other workers for surface soil layers. The sum of different soil-nitrogen fractions were always higher than the total nitrogen in soil.     

Nitrification in some tropical soils

Summary Nitrification of soil N in 8 mineral and 2 histosols having a wide range in pH (3.4 to 8.6), organic C (1.22 to 22.70%) and total N (0.09 to 1.20%) was studied by measuring nitrate fromation under aerobic incubation of the soil samples at 30°C for 4 weeks. The amounts of NO₃-N produced in the soils varied from 0 to 123 μg/g of soil. Soil N in the two acid sulfate soils and one other acid soil did not nitrify under conditions that stimulate nitrification. Soils having pH more than 6.0 nitrified at a rapid rate and released NO₃-N ranging from 98 to 123 μg/g. The two organic soils differed considerably in their capacity to nitrify though the total amounts of mineral N released were similar in these soils. The amounts of NO₃-N formed in the soils was highly positively correlated with the soil pH but was not significantly correlated with the organic C of total N content of the soils. Statistical analysis also showed that nitrate formation was not significantly correlated with soil pH in soils having pH higher than 6.0.     

Totalsulfur,acetate-extractable sulfur and isotopically exchangeable sulfate in some eastern canadian soils

Summary Although S-deficiencies are not found in Eastern Canada, the possibilities of potential S-deficiencies exist. Total acetate-extractable S and isotopically-exchangeable SO₄ was determined on selected Eastern Canadian soils.Total S varied from 0.008 to 0.207 per cent and was not related to geographic location or soil use. Extractable S varied from 11 to 144 µg S per gram of soil and was generally highest in B- and calcareous C-horizons. Isotopically-exchangeable SO₄ ranged from 0.64 to 9.9 µg S per gram of soil, the larger value occurring in the B-horizon soil samples.Sulfur values were greater than those found in deficient soils elsewhere.Contribution from the Departments of Soil Science and Agricultural Chemistry, Macdonald College of McGill University, Quebec, Canada.Assistant Professor, Professor Emeritus, and graduate student respectively. The authors gratefully acknowledge the support of the Government of the United Arab Republic in the form of a scholarship to I.S.C.     

Total, organic and extractable-P in humus and soil beneath Sitka spruce planted in pure stands and in mixture with Scots pine

Total, organic and extractable P were measured in the humus and underlying soil to 10 cm depth beneath Sitka spruce (SS) and mixed Sitka spruce and Scots pine (SS+SP) stands planted on upland heath. The humus beneath SS+SP contained significantly (p<0.01) greater amounts of total and organic-P than that in SS and the mixed stands had more effectively retained approximately 87 per cent of previously applied fertilizer-P, totalling 100 kg P ha^–1, compared with 70 per cent in SS. Despite the larger amounts of total-P in the mixed plots 0.01 M CaCl₂ extractable molybdate reactive phosphorus (MRP) was significantly (p<0.05) greater in SS+SP humus only during March and April. Greater concentrations of MRP were released from the humus and soil during July and August at a mean rate of 58 g P ha^–1 day^–1. This coincided with drying of the soil during the summer and the rate of release, attributed to death of fine roots and microorganisms, was 4 to 30 times greater than reported values for rates of net mineralization of P from forest soils.     

湖南主要类型稻田土壤固定态铵含量及其影响因素

通过野外调查取样和室内培养试验 ,应用Silva和Bremner方法 ,研究了湖南省主要类型稻田土壤的固定态铵含量及其影响因素 .结果表明 ,该省主要类型稻田土壤固定态铵含量为 141～ 35 3mg·kg-1,平均为 2 72± 6 7mg·kg-1,占土壤全N的 11.2 % ,高于湖南省以北各地区土壤和本地区地带性土壤———红壤的固定态铵含量 .其含量的顺序为河沙泥 >紫泥田 >潮沙泥 >黄泥田 >红黄泥 .在土壤剖面中 ,固定态铵含量随剖面深度的变化有 4种情况 :在 1m深度范围内随深度增加而增加 ;随深度增加而减少 ;随深度增加而无明显变化 ;土壤剖面中某一土层固定态铵含量明显增加或减少 .土壤固定态铵含量占土壤全N百分比随深度增加而恒增大 .土壤对NH+ 4的固定作用在 30℃下最强 ,高于 2 0℃和 40℃ ;长期淹水有利于潮沙泥、紫泥田和河沙泥对NH+ 4的固定作用 ,但干湿交替有利于黄泥田对NH+ 4的固定作用 .相关分析表明 ,土壤固定态铵含量仅与 <0 .0 1mm粘粒含量呈P0 .0 5水平的显著正相关 ,与有机质、全N、有机N和 <0 .0 0 1mm粘粒含量的相关性均不显著     

Non-exchangeable binding of ammonium and amino nitrogen by Norway spruce raw humus

Summary The capacity of an originally acid Norway spruce raw humus to fix isotopically labelled ammonium and amino nitrogen in a form resistant to cold 1N HCl treatment was studied. The amount fixed was determined after a reaction period of 24 hours (the humus pretreated with propylene oxide), using the amount of labelled N in the HCl-leached humus residue as a basis for calculating the amount of added N fixed. The nitrogen sources used were ammonium chloride, glycine and cyanamide. It was found that the fixation of added ammonium and glycine N was exceedingly low in the H⁺-saturated raw humus (pH 3.3–3.4), but the fixation rate was rapidly increased by increasing the pH during the aerobic incubation. Maximum fixation was obtained at a final pH of 10–11. Within the acid range the fixation was constantly higher for added glycine-N than ammonium-N. On the alkaline side of the neutral point the amount of fixation tended to be similar for ammonium and glycine. In treatments with N¹⁵-labelled ammonium, it was shown that small but fully detectable amount of added N were present in the soluble organic N fraction of the HCl extract, the quantities increasing with increasing soil pH during the incubation. The fixation was increased by increasing temperature and decreased by oxidative pretreatment of the humus before the addition of N. In the nitrogen gas atmosphere the fixation figures were 40 to 50 per cent lower than for corresponding treatments in air atmosphere. When various N compounds were added in equimolar concentrations the highest fixation was recorded for cyanamide. In studying the stability of fixed N to acid hydrolysis, it was found that 54 per cent of the fixed N resisted eight hours' refluxing with 6N HCl, the corresponding figure for the native raw humus N being 19 per cent. About one third of the fixed N was liberated as ammonia during the acid hydrolysis.     

Muskegon Wastewater Land Treatment System: Fate and Transport of Phosphorus in Soils and Life Expectancy of the System

The build‐up of phosphorus (P) in soil is a major factor limiting the operating life of a wastewater land treatment system. In this study, effects of long‐term wastewater application on changes in chemical properties, P profiles, and P adsorption capacity were evaluated in soils of the Muskegon wastewater land treatment plant that has been treating wastewater for > 30 years. Results indicate that the major soil properties have been changed. In the 15 cm topsoil, the pH increased from ～ 5–6 in 1973 to ～ 7.4–7.8 in 2003; the soil's total organic carbon (TOC) increased by 10–71 %; and the level of exchangeable Ca in 2003 is 8–9 times higher than that in 1973. The amount of Ca/Mg absorbed in the soil affects the P adsorption capability of the soil; Ca‐ and Mg‐bound P accounts for > 70 % of the total P adsorbed in the soil. The net P accumulated in the Rubicon soil increased from ～ 700 in 1993 to ～ 1345 kg/ha soil in 2001, but the plant available P varied between ～ 100–500 kg/ha soil during the same period, indicating a large amount of the applied P has become the fixed P that is unavailable to plants. P sorption in the soil consists of a fast adsorption and a slow transformation process. The soil's maximum P sorption capacity (P_max) (based on 1‐day isotherm tests) has been increased by ～ 2–4 times since 1973; the actual P_max of the Muskegon soils could be much higher than the 1‐day P_max. Therefore, the life expectancy of the Muskegon system has been extended significantly with the application of wastewater.     

Mechanistic Analysis of Ammonium Inhibition of Atmospheric Methane Consumption in Forest Soils

Methane consumption by forest soil was studied in situ and in vitro with respect to responses to nitrogen additions at atmospheric and elevated methane concentrations. Methane concentrations in intact soil decreased continuously from atmospheric levels at the surface to 0.5 ppm at a depth of 14 cm. The consumption rate of atmospheric methane in soils, however, was highest in the 4- to 8-cm depth interval (2.9 nmol per g of dry soil per day), with much lower activities below and above this zone. In contrast, extractable ammonium and nitrate concentrations were highest in the surface layer (0 to 2 cm; 22 and 1.6 μmol per g of dry soil, respectively), as was potential ammonium-oxidizing activity (19 nmol per g of dry soil per day). The difference in zonation between ammonium oxidation and methane consumption suggested that ammonia-oxidizing bacteria did not contribute significantly to atmospheric methane consumption. Exogenous ammonium inhibited methane consumption in situ and in vitro, but the pattern of inhibition did not conform to expectations based on simple competition between ammonia and methane for methane monooxygenase. The extent of ammonium inhibition increased with increasing methane concentration. Inhibition by a single ammonium addition remained constant over a period of 39 days. In addition, nitrite, the end product of methanotrophic ammonia oxidation, was a more effective inhibitor of methane consumption than ammonium. Factors that stimulated ammonium oxidation in soil, e.g., elevated methane concentrations and the availability of cosubstrates such as formate, methanol, or β-hydroxybutyrate, enhanced ammonium inhibition of methane oxidation, probably as a result of enhanced nitrite production.     

Availability of Ca from Ca45SO4 in a highly saline-sodic soil

Summary Application of gypsum (tagged Ca⁴⁵SO₄.2H₂O) caused a considerable increase in dry matter yield and content of Ca, Ca⁴⁵, Mg and K and Ca:Na and (Ca+Mg): (Na+K) ratios and a decrease in the content of Na, N and P in dhaincha tops. There was a considerable increase in the total uptake of Ca, Mg, Na, K, N, P and Ca⁴⁵ by plant tops in response to gypsum. Contribution of Ca from applied Ca⁴⁵SO₄ varied from 78.3 to 84.7 per cent of the total Ca in plant tops, whereas, its uptake from this source varied from 52.18 to 98.73 me per 100 g plant tops. re]19720705     

The effect of ferrous sulphate on the yield and manganese uptake of oats on sandy soil fertilized with natural pyrolusite

Summary The effects of soil treatments with ferrous sulphate and an equivalent amount of hydroquinone on the yield of dry matter and the manganese uptake of oats were investigated in pot experiments using a sandy soil deficient in manganese, with and without additions of finely ground, natural pyrolusite containing some manganite.In soil not fertilized with pyrolusite an application of hydroquinone gave a higher yield of dry matter and a considerably higher manganese uptake than an application of the equivalent quantity of ferrous sulphate.In soil fertilized with hydroquinone an increase of 23 per cent in the yield of dry matter and an increase of 50 per cent in the manganese uptake per pot were found when the soil was fertilized with 100 g of natural pyrolusite <50µ per pot. In soil fertilized with a quantity of ferrous sulphate equivalent to hydroquinone, an increase of 21 percent in the yield of dry matter and an increase of about 200 per cent in the manganese uptake per pot were found when the 100 g of pyrolusite was applied.     

Mineralization and gaseous losses of nitrogen from urea and ammonium sulphate in salt-affected soils

Summary An incubation study on mineralization and gaseous losses of nitrogen was conducted on three soils with increasing levels (1.1 to 50 mmhos/cm) of salinity and two levels of urea and ammonium sulphate upto 6 weeks. Mineralization of nitrogen increased with time and decreased with the increase of salinity. It was more from ammonium sulphate than urea, and relatively more from the lower dose. The gaseous losses of NH₄-N increased with salinity. About 35±5 per cent of added N was lost in the gaseous form at maximum (ECe=45 to 50 mmhos/cm) salinity and losses were more from light than heavier soils. Salinity and pH, both were correlated negatively with the N mineralisation and positively with the gaseous losses of ammonia in these salt-affected soils. re]19751105     

Effect of soil solution phosphorus in Volcanic Ash soils on the response of tomato (Lycopersicum esculentum) to added phosphate

Summary Sorption isotherms of six Volcanic Ash soils were used to determine Optimum P, i.e. the amount of added P required to produce a soil solution concentration of 0.2 µg P per ml. In a pot test, application of these amounts of P to the soils led to maximum or near maximum growth of tomato plants, (Lycopersicum esculentum), harvested at 35 days. After harvest the soil solution concentration of P in all the soils had fallen below 0.2 µg per ml whatever the rate of P added initially. The amount of P required to restore the soil solution to 0.2 µg P per ml was linearly related to the fertilizer P originally applied to the soil; the higher the P applied originally the lower was the future P requirement. The regression coefficients suggested that the applied P would be twice as effective at reducing subsequent P requirement in a Recent Volcanic Ash soil than in the other more developed soils. Measurement of extractable Al (NH₄OAc at pH 4.2) showed that lack of growth at low levels of added P on a high P fixing soil could be caused by insufficient P due to high levels of Al, although with a soil of pH 6 this would not have been expected. re]19760217     

Nitrogen balance studies for different Egyptian soils cropped with corn

Summary The nitrogen balance for four different Egyptian soils cropped with corn and fertilized with increasing amounts of ammonium sulphate was studied in pot experiments. The tested soils were clay loam, calcareous sandy loam, sandy loam and sand. Nitrogen added as seeds, fertilizers, irrigation water and insecticides, nitrogen removed by the plants including thinned plants and fallen leaves and the nitrogen content of the soils before sowing and after the harvest were determined and used to draw the balance sheet.The obtained results showed that nitrogen loss ranged between 6.8 and 51.5 per cent depending mainly on soil type and to some extent on the rate of applied ammonium sulphate. Nitrogen uptake by the corn plants was lowest from the clay loam soil and highest from the sandy soil. In all cases it increased slightly with the addition of nitrogen fertilizer. re]19720918     

Nitrification in soils of secondary vegetational successions from Eucalyptus forest and grassland to cool temperate rainforest in Tasmania

Rates of nitrification in well drained granitic soils from forest stands and grassland of differing successional status and from beneath isolated individuals of several tree species were compared in a series of laboratory experiments. Fresh samples were perfused with distilled water or nutrient solution for 10 to 14 weeks at 20°C. The following treatments were applied to the soils singly and in combination: 200 and 400 g N g^–1 as (NH₄)₂SO₄; 100 g P g^–1 as KH₂PO₄; 4000 g CaCO₃ g^–1; inoculation of non-nitrifying soil with nitrifying soil; perfusion of nitrifying soil with leachate from non-nitrifying soil.Nitrification was absent or occurred at only a low rate in many soils; it generally increased as succession proceeded from nature grassland or eucalypt forest towards climax temperate rainforest, but decreased in mature climax forests. However, the influence of individual tree species was often paramount. Nitrification was stimulated by disturbance of a stand by disease. A possible inhibitor of nitrification in a rainforest soil could not be removed by leaching with water, nor transferred via the leachate to a nitrifying soil. Addition of P was without effect on either total amount of nitrate produced or on net mineralisation of soil N, but sometimes increased the rate of nitrification of added ammonium. Non-nitrifying rainforest soil of pH 4.3 was induced to nitrify only after addition of (NH₄)₂SO₄, inoculation with a nitrifying soil, and addition of CaCO₃ to raise pH by 3 units. However, once nitrification had commenced it could continue with little change in rate while pH decreased to a value of 3.4.It was concluded that rate of nitrification is dependent upon the presence of particular tree species in a stand, upon its history of disturbance, and hence in part upon the stand's successional status. It is not limited by pHper se within the range found in these soils, although an increase in pH may be necessary to initiate nitrification. In some soils the rate of nitrification may be limited by the level of ammonium substrate, and nitrifiers are virtually absent from others. Overall microbial activity is limited by lack of utilisable carbon substrate.