Inhibitory effects of commercial potassium chloride on the nitrification rates of added ammonium sulphate in an acid red yellow podzolic soil

Summary Rates of nitrification of ammonium sulphate in an acid red yellow podzolic tea soil in Sri Lanka with and without the addition of commercial potassium choride (95% KCl) and analytical grade KCl was studied under field conditions and in a laboratory incubation experiment. Addition of KCl effectively suppressed nitrification and this suppression was found to be due to the presence of Cl-ions rather than K-ions.     

Response of barley and wheat to phosphorus in the presence of chloride and sulphate salinity

Summary The study was conducted in a greenhouse and under field conditions. In the greenoouse, barley was grown to maturity in pots on a sandy soil which contained 80 and 120 meq/l of chloride and sulphate dominant salts in its saturation extract, to which 0, 10, 25 and 50 ppm P were added. In the field study, wheat was grown on loamy sand soils having 0, 25, 50 and 75 kg/ha added P levels and irrigated with either Cl- or SO₄-dominant saline waters (EC=15–19 mmhos/cm). The results of the greenhouse study indicated that at maturity barley straw and grain yield was significantly increased by 50 ppm of added P both on the non-saline control and the Cl-treatments. However, 25 ppm P was optimal on the SO₄-treatments. The Cl content of plants was significantly decreased and S was increased with the increase in the P content of soil. A synergistic relation between the S and P content of barley shoots was observed. In the field study wheat grain yield responded significantly to P applications upto 50 kg/ha level on the Cl-site and there was no response to applied P on the SO₄-site, although the former contained more Olsen's P than the latter. The results suggested that P requirement of wheat and barley was greater on Cl- than on SO₄-salinity.     

双氰胺对碳酸氢铵在土壤中氮素转化的影响

采用室内培养试验方法,研究了双氰胺对碳酸氢铵中的铵态氮在土壤中动态变化的影响。结果表明,无论是碳铵与双氰胺的机械混施,还是含双氰胺的长效碳铵,在抑制铵态氮硝化产生硝态氮的同时对氨挥发也有一定的抑制作用,使土壤在更长的时间内保持更高的铵态氮含量,并对碳铵施入后土壤的酸碱化强度起到了缓冲作用。添加双氰胺不但提高了碳铵的氮肥利用率,还减少了肥料氮素损失.     

Response of plants to calcium concentration in flowing solution culture with chloride or sulphate as the counter-ion

Summary Solution calcium concentrations required for the growth of a range of plant species, including both monocotyledons and dicotyledons, were determined in two experiments in which plants were grown in flowing solution culture at constantly maintained calcium concentrations ranging from 0.5 to 3000 μM. Calcium chloride was used as the calcium source in the first experiment, calcium sulphate was used in the second. At calcium concentrations of 10 μM and below, all species developed calcium deficiency symptoms. The severity of the deficiency was more pronounced in the dicotyledons than in the monocotyledons. However, cassava was much more tolerant than all other dicotyledons and equally as tolerant as rice, the most tolerant monocotyledon. Solution calcium concentrations required for 90% of maximum yield were generally lower for monocotyledons (3 to 20 μM) than for dicotyledons (7 to 720μM) when calcium chloride was used as the calcium source. When calcium sulphate was used, 7 out of 11 species, including 3 monocotyledons, required external calcium concentrations of 1200 μM and above. The results are discussed in relation to effects of solution composition and the choice of counter-ions on plant response to calcium and other macronutrient cations. It is concluded that yield depressions due to toxicity of excesses of chloride, and possibly other counter-ions, can lead to serious underestimation of limiting external cation concentrations for plant growth.     

Nitrate reductase activity and growth response of forest species to ammonium and nitrate sources of nitrogen

Summary Three tree species,Eucalyptus regnans (F. Muell.),E. obliqua (L'Herit.),Pinus radiata (D. Don) were grown in sand culture with different proportions of nitrate and ammonium. Nitrate Reductase Activity (NRA) was induced in root tissue of all species and in leaf tissue of the eucalypts. An increasing proportion of nitrate resulted in increasing NRA in all species and hence NRA alone is no indication of N-preference. The highest NRA was found withE. regnans, a result which has also been obtained in the mature forest. The growth ofE. regnans was least with NH₄ ⁺ alone, whereas that ofE. obliqua was least with NO₃ ^– alone. The soils of matureE. regnans forest have a high potential for nitrification while those ofE. obliqua forest show little nitrification. Thus the preference for particular N sources shown by seedlings in culture is supported by related properties of mature forests. It is postulated however, that the inducibility of a high level of RNA in seedlings is more likely a result of a preference for NO₃ ^– than a cause.     

Plant, soil microbial and soil inorganic nitrogen responses to elevated CO2: a study in microcosms of Holcus lanatus

The impact of elevated atmospheric CO₂ concentrations on the nitrogen cycle was evaluated in a 2-month experiment in monospecific grassland microcosms (Holcus lanatus L.) grown on reconstituted grassland soil. The responses of the N pools in the plants, soil, and soil microbes were studied. The impact of high CO₂ on key stages of the N cycle, especially nitrification and denitrification processes, were also measured. Our study showed a strong plant response to high CO₂: total biomass increased by 76% (P < 0.001) and root length density increased by 77% (P = 0.010). However, total plant N was not significantly modified by high CO₂, because the percent N in the plant decreased by 40% (P < 0.001). We observed a large decrease in soil NO₃^– concentration under elevated CO₂ (–50%; P = 0.002). Soil ammonium concentrations were much less affected by CO₂ enrichment, and only in resin bags (–8%, P = 0.019). Soil nitrifying enzyme activity (NEA) had a tendency to increase (+17%; P = 0.061) and denitrifying enzyme activity (DEA) decreased (-12%; P = 0.013). We found evidence of increased microbial N sink (microbial N increased by 17%, P = 0.004). This and other studies suggest that rising CO₂ often reduces soil nitrate concentrations, which may lead to decreased nitrate leaching. Elevated CO₂ led to environmental conditions that were less favourable for denitrification in our study.     

Transformation of urea and ammonium sulphate in different soils

Summary The transformation of urea and ammonium sulphate in Ladwa sandy loam and Balsamand sand was studied in laboratory. Urea took at least one week in sandy loam and 2 weeks in sandy soils to hydrolyse completely. The process of hydrolysis was faster in finer soil with high organic matter than in coarse soil having low organic matter. There was no nitrification upto 3 days in sandy loam and upto 7 days in sandy soils, respectively, but there was immobilization of NO₃-N during these initial periods. The NO₃-N content at the end of incubation period (35 days) was more in case of urea than in case of ammonium sulphate treated samples in sandy loam soil and reverse was true in sandy soil. The hydrolysis of urea did not follow zero or first order kinetics as proposed in previous studies.     

Effects of residual soil salinity resulting from irrigation with sulphate waters on lettuce

Summary The response of lettuce (Lactuca sativa L.) to residual soil salinity as influenced by the ionic composition of two different saline waters (EC_w=3.1 dS/m, referenced at 25°C) and rain water, was investigated in a greenhouse experiment with three successive plantings of lettuce in the same soil. One of the saline waters was saturated with gypsum (SO₄=35 mol (−)m⁻³) and the other contained SO₄ at 15 mol (−)m⁻³ and Na and Cl at 18 and 14 mol (±)m⁻³, respectively (mixed water). All waters were applied with a 0.3 leaching fraction. Soil water salinity and sodium adsorption ratio (SAR) increased in both cases using saline waters. The effect of mixed saline water was higher and became more marked after each planting, resulting from higher contribution of Na and Cl to soil salinity. With both saline waters, soil solution became saturated with gypsum. At first planting, gypsum saturated and mixed waters produced fresh yield increases of 15 and 24%, respectively, relative to rain water. At second planting, however, there was reduction in yield of 11 and 22%, respectively, relative to rain water; at third planting yield reduced by 22 and 76% with gypsum saturated and mixed water, respectively.     

Alleviating soil sickness caused by aerobic monocropping: responses of aerobic rice to soil oven-heating

“Aerobic rice” system is the cultivation of nutrient-responsive cultivars in nonflooded and nonsaturated soil under supplemental irrigation. It is intended for lowland areas with water shortage and for favorable upland areas with access to supplementary irrigation. Yield decline caused by soil sickness has been reported with continuous monocropping of aerobic rice grown under nonflooded conditions. The objective of this study was to determine the growth response of rice plant to oven heating of soil with a monocropping history of aerobic rice. A series of pot experiments was conducted with soils from fields where rice has been grown continuously under aerobic or anaerobic (flooded) conditions. Soil was oven heated at different temperatures and for various durations. Plants of Apo, an upland variety that does relatively well under the aerobic conditions of lowland, were grown aerobically without fertilizer inputs in all six experiments. Plants were sampled during vegetative stage to determine stem number, plant height, leaf area, and total biomass. Heating of soil increased plant growth greatly in soils with an aerobic history but a relatively small increase was observed in soils with a flooded history as these plants nearly reached optimum growth. A growth increase with continuous aerobic soil was already observed with heating at 90°C for 12 h and at 120°C for as short as 3 h. Maximum plant growth response was observed with heating at 120°C for 12 h. Leaf area was most sensitive to soil heating, followed by total biomass and stem number. We conclude that soil heating provides a simple and quick test to determine whether a soil has any sign of sickness that is caused by continuous cropping of aerobic rice.     

Response of coastal phytoplankton to ammonium and nitrate pulses: seasonal variations of nitrogen uptake and regeneration

Seasonal variation in uptake and regeneration of ammonium and nitrate in a coastal lagoon was studied using ¹⁵N incorporation in particulate matter and by measuring changes in particulate nitrogen. Uptake and regeneration rates were two orders of magnitude lower in winter than in summer. Summer uptake values were 2.8 and 2.2 mol N.l^–1.d^–1 for ammonium and nitrate, respectively. Regeneration rates were 2.9 and 2.1 mol N.l^–1.d^–1 for ammonium and nitrate respectively. Regeneration/uptake ratios were often below one, indicating that water column processes were not sufficient to satisfy the phytoplankton nitrogen demand. This implies a role of other sources of nitrogen, such as macrofauna (oysters and epibionts) and sediment. Phytoplankton was well adapted to the seasonal variations in resources, with mixotrophic dinoflagellates dominant in winter, and fast growing diatoms in summer. In winter and spring, ammonium was clearly preferred to nitrate as a nitrogen source, but nitrate was an important nitrogen source in summer because of high nitrification rates. Despite low nutrient levels, the high rates of nitrogen regeneration in summer as well as the simultaneous uptake of nitrate and ammonium allow high phytoplankton growth rates which in turn enable high oyster production.     

Nitrification inhibition of added nitrogenous fertilisers by potassium chloride in soil

Summary Inhibitory effect of potassium chloride on nitrification of ammonium sulfate and urea in acid, neutral and calcareous soils was observed in an incubation study. In acidic soil, NO ₃ ^– –N production in soil treated with urea was retarded by addition of KCl. NO ₃ ^– –N concentration was much less even in comparison to control where ammonium sulfate and KCl were added together which might be due to cumulative effect of Cl^– and SO ₄ ^–2 ions. In neutral and calcareous soils, nitrification inhibition was less conspicuous.     

Effects of parathion and malathion on transformations of urea and ammonium sulfate nitrogen in soils

Summary A study of the effects of malathion and parathion applied at 10 and 50 g/g of soil on transformations of urea and (NH₄)₂SO₄–N in a sandy loam showed that the insecticides retarded urea hydrolysis as well as nitrification of urea and (NH₄)₂SO₄–N. At 50 parts/10⁶ rate of the insecticides, inhibition of urea hydrolysis ranged from 44 to 61% after 0.5 week and from 7 to 21% after 3 weeks of application. The insecticides inhibited the conversion of NH₄ ⁺ to NO₂ ^– without appreciably affecting the subsequent oxidation of NO₂ ^– to NO₃ ^– –N. This resulted in accumulation of higher amounts of NH₄ ⁺–N in soil samples treated with ammonium sulfate or urea N.The results suggest that transformations of urea and NH₄ ⁺ fertilizers in soils may be influenced by the amount of organophosphorus insecticide present and this may affect plant nutrition and fertilizer use.     

Specific ion effect as a probable cause of growth inhibition under saline conditions

Summary The replacement of carboxy-proton of IAA, plays an important role in the process of growth under saline conditions. Appreciable changes in pH have ben observed in the presence of CO₃ ^–2 and HCO₃ ^–, and increase in pH appears to be caused owing to the formation of unstable complex of IAA, which soon hydrolyzes and gives alkalinity. The pH change thus achieved favours IAA oxidase activity; therefore, suppression of growth is resulted in CO₃ ^–2 and HCO₃ ^– medium. In the presence of SO₄ ^–2 and Cl^– salts slight lowering of pH takes place which does not favour IAA oxidase activity. It is therefore, presumed that anion (CO₃ ^–2, HCO₃ ^–, SO₄ ^–2 and Cl^–) controls the process of growth and development through the alteration of pH of the medium.     

Controls on inorganic N species transformations and potential leaching in freely drained sub-soils of heavily N-impacted acid grassland

In N-polluted, minimally managed soils, recent research has shown that ammonium-N, as well as nitrate-N, may move down through soil profiles. There is a need, therefore, to reassess what controls N species transformations below the rooting depth in such soils. The changes with depth down to 1 m in extractable ammonium-N and nitrate-N concentrations have been studied for two heavily N-impacted acid grassland soils near York, UK, for fresh soils and for soils incubated after either deionised water (d.w.) or ammonium-N spiking. Although in close proximity, the profiles showed marked differences in their relationships of ammonium- and nitrate-N to soil pH, C%, N% and C:N ratio. One profile was slightly more acidic at the surface, which seems to have changed the distribution of organic matter throughout the soil profile. Trends in ammonium production with depth were clearer when ammonium-N concentrations were recalculated on the basis of ammonium-N per unit mass of soil organic C. This then allowed a consistent trend with soil pH to be discerned for both profiles. Ammonium-N spiking showed that ammonium substrate availability was limiting potential net nitrification rate at 20–60 cm depth for both profiles. Potential mineral-N production was considerable at depth, which would facilitate transport of N to surface waters and/or groundwaters.     

Effect of sulphate waters on soil salinity,growth and yield of tomatoes

Summary Tomato (Lycopersicon esculentum var. VF 145) plants were grown with three soils in a greenhouse irrigated with water high in sulphates to determine their effects on soil salinity, growth and yield. Fruit fresh weights decreased by 53 and 40% when irrigated with water having 32 and 16 meq SO₄/l respectively, and no leaching was allowed, relative to irrigating with a half strength modified Hoagland solution. When a 0.3 leaching fraction was allowed the respective decrease in fruit fresh weights were 32 and 12% for the two levels of sulphate. Tops were less affected than were fruits. The electrical conductivity of solutions extracted from the soils during the growing period was highly correlated with the soil solution SAR (sodium adsorption ratio) and with Na and Cl concentrations. Leaching, although effective in controlling soil salinity caused by highly soluble salts, was ineffective in controlling salinity derived from SO₄.     

水稻根系生长及其对土壤紧密度的反应

采用筒栽方法研究了杂交稻汕优63和65002在分蘖期,穗分化期,开花期和成熟期根系生长量和垂直分布以及开花期土壤容重对根系生长和分布的影响,结果表明,根系生长量以开花期最高,开花后下降,随生育进展,深层根系（20-45cm)比例提高,分蘖期到穗 分化期是根系重量增长最快,且根系向下生长的主要时期,随耕层以下土壤容重提高,根系生长量下降,同时深层根系比例下降。     

Identification and study of growth and nitrogenase activity of nitrogen fixing cyanobacteria from tropical soil

Identification of cyanobacteria species has been performed on samples coming from two different harvest areas. The most important fixing belongs to Scytonema genus. The other genus identified are Nostoc and Lyngbia. Moreover, these cells are living closely with non-fixing cyanobacteria as well as with bacteria. The growth of cells as well as nitrogenase activity has been studied on a semi-axenic strain of Scytonema, a nitrogen fixing cyanobacterium, isolated from soil crusts. The cell growth is relatively show in liquid medium depleted in combined nitrogen. The growth rate increases when nitrates are supplied to cells. A release of ammonium is observed in medium during cell culture. This release exhibits several maxima and minima during cell growth. The heterocyst cells disappear within four days when filaments are growing in nitrates supplied medium. On the contrary, the heterocyst frequency increases up to more 5% in a nitrogen depleted medium. The heterocyst frequency reaches a maxima after 4 days of culture, then decreases later on. Nitrogenase activity changes during cells growth too. The maximum activity is observed after 5 to 6 days of culture to decrease after even though the cells are still in their exponential phase of growth. Nitrogenase activity increases with light intensity, what indicate a possible relation between photosynthetic and nitrogenase activities.     

Theoretical considerations on growth kinetics and physiological adaptation of nutrient-limited phytoplankton

In many experimental ecological studies on phytoplankton species the growth response of an organism to the prevailing environmental conditions have been studied. Curves relating specific growth rate () to the external nutrient concentration (S) have been constructed to compare nutrient-limited growth of different species under steady state conditions. Microorganisms adapt their physiology to a certain limitation in order to optimize growth. Therefore the shape of the /S curve is closely related to the way a micoorganism adapts its physiology. To see how physiological adaptation and growth rate are interconnected to each other, both can be related to the internal concentration of the growth-limiting nutrient. How the growth rate is related to the internal nutrient concentration is presented in a mathematical equation.Many phytoplankton species during growth under different nutrient limitations show a linear relationship between and the reciprocal value of the internal nutrient content (= Yield). This was originally observed by Droop. The model presented here gives a theoretical explanation of this phenomenon.     

The effect of air-borne ammonium sulphate onPinus nigra var.maritima in the Netherlands

Summary As a result of air pollution, considerable deposition of ammonium sulphate occurs on vegetation and soil in the vicinity of chicken farms and fields dressed with animal slurry. A clear relation exists between this ammonium sulphate deposition and the distance to certain agricultural activities. Field investigations and ecophysiological experiments both show that the needles ofPinus nigra var.maritima (Ait.) Melville take up ammonium and excrete potassium, magnesium and calcium. This often results in potassium and/or magnesium deficiencies and may lead to premature shedding of needles. The high levels of nitrogen in the needles are strongly correlated to fungal diseases.Whether the observed cation leaching will result in disturbed nutrient budgets depends mainly on soil conditions. Leaching of K, Mg and Ca from the soil, caused by ammonium sulphate, may further inhibit nutrient uptake.Field investigations show a clear correlation between increased ratios of NH₄ to K, Mg and Ca in the soil solution and the damage to pine forests.