The Effect of Soil pH on Nitrification in Coarse Sandy Soil

Author(s):  
Finn P. Vinther ◽  
Finn Eiland
Keyword(s):  
Soil Ph ◽  
1970 ◽  
Vol 75 (3) ◽  
pp. 571-576 ◽  
Author(s):  
A. Islam ◽  
J. Bolton

Ryegrass was used to remove potassium from two acid soils limed to different pH values. Most non-exchangeable potassium was removed from the unlimed soils (pH 4·5) but differences in removal between pH 5·5 and 7·0 were small. Air-drying the soils after cropping released further potassium into the exchangeable form in amounts independent of soil pH.Equilibrium potassium activity ratios (ARK) after each out declined to small constant values characteristic of the soils. A sandy soil (Woburn) initially contained less exchangeable potassium than a soil with more clay (Sawyers), but after a few crops, ARK, % K in the grass and K uptakes per cut were larger from Woburn soil, showing that non-exchangeable potassium was being released faster than in the other soil.


1986 ◽  
Vol 34 (1) ◽  
pp. 103-106
Author(s):  
H. Niers ◽  
J. van der Boon

Eight field trials were carried out with various heather cultivars (Calluna vulgaris Carmen, Cuprea, Robert Chapman; Erica tetralix Con Underwood; E. carnea [herbacea] King George and E. cinerea C.D. Eason). Peat at 0-8 msuperscript 3/100 msuperscript 2 was incorporated into the top soil or applied as a layer and soil pH-KCl was maintained at levels between 3 and 6.8. Increasing peat application up to 4 msuperscript 3/100 msuperscript 2 improved the growth and quality (visual rating) of the stand; higher amounts had little additional effect. Peat applied as a layer gave some slightly better results than peat incorporated into the topsoil. A soil pH-KCl value of 4.2 was the optimum for growth of most cultivars and reasonable growth could be expected in the range 3.8-4.7. Cv. King George was more tolerant to high pH than cultivars of the other species tested. In 3 trials with Calluna cultivars MgO application at 150 or 200 kg/ha increased the Mg content of the soil and shoots but had a slight negative effect on growth. (Abstract retrieved from CAB Abstracts by CABI’s permission)


Author(s):  
M. Esper Neto ◽  
C. F. Coneglian ◽  
A. C. S. Costa ◽  
T. T. Inoue ◽  
M. A. Batista

Lime application is the most appropriate technique to raise soil pH, decrease Al3+ toxicity and increase Ca2+ and Mg2+ contents in acidic tropical and subtropical moist soils. The objective of this research is to evaluate changes in chemical attributes and soybean yield in sandy soil after lime incorporation. The soil was classified as a typical Quartzipsamments cultivated with (Brachiaria decumbens Stapf) pasture, and its degradation state was classified as strong. The experimental design was a randomized block with six replicates and four lime doses (0, 2, 4 and 8 Mg ha-1). The soil in the area was prepared with one plowing and two harrowings, followed by lime application and two more harrowings to incorporate the lime up to 0.2 m depth. The dependent variables analyzed were soybean yield; numbers of pods filled, pods not filled, and total pods and soil pH in water, CaCl2 and KCl. All parameters were measured at depth of 0.0-0.1, 0.1-0.2 and 0.2-0.3 m. The increase of soil pH by the different lime rates were observed just in 0.0-0.1 and 0.1-0.2 m layers. After 6 months no changes in soil pH were observed in subsoil (0.2-0.3 m). With lower H+ and Al3+ activity and higher basic cation availability, soybean yield was also changed. The maximum soybean yield of 2,929 kg ha-1 was observed with 4.6 Mg ha-1 lime application, although pod number per plant remained constant, independent of limestone dose.


Agronomy ◽  
2021 ◽  
Vol 11 (3) ◽  
pp. 525 ◽  
Author(s):  
João William Bossolani ◽  
Luiz Gustavo Moretti ◽  
José Roberto Portugal ◽  
Ricardo Rossi ◽  
Carlos Alexandre Costa Crusciol

This study explores whether Thermomagnesium (TM), a by-product of Ni ore mining, is an efficient fertilizer for maize. The effects of TM on soil pH, the supply of Si and Mg to the soil and plants, carbohydrate metabolism, grain filling, and yield were assessed in two simultaneous experiments performed in greenhouse conditions. Five TM doses were applied to two soil textures—clayey (0, 55, 273, 709, and 2018 mg kg−1) and sandy (0, 293, 410, 645, and 1260 mg kg−1). In general, the best results in soil and maize plants occurred at the highest TM dose for both soil textures (clayey 2018 mg kg−1 and sandy 1260 mg kg−1). The results demonstrated that in both soils, the concentrations of Mg and Si in the maize leaves increased with the dose of TM, similarly to that which occurred in the soil. Interestingly, in clayey soil, the soil pH increased linearly, whereas in sandy soil, the pH reached its maximum value between the two largest TM doses. The concentration of reducing sugars increased at the highest TM dose, whereas the concentrations of sucrose and starch decreased. The enhancement of carbohydrate partitioning led to higher maize growth, grain filling, and yield. Overall, the results clearly demonstrate that TM is a sustainable alternative fertilizer for maize and can be used for countless other crops and soil classifications, thus providing a suitable destination for this by-product of Ni ore mining.


2019 ◽  
pp. 405-412
Author(s):  
Aare Selberg ◽  
Jana Budashova ◽  
Kalev Uiga ◽  
Toomas Tenno

Surfactants are applied as emulsifiers or solubilizers by treatment of polluted soil. Theproblem of secondary pollution has arisen as result of the surfactant-enhanced remediation ofa polluted soil contaminated with hydrophobic organic compounds. Several studies haveshown that the surfactants are biodegradable in aerobic conditions and the biodegradabilitydepended on the chemical properties and concentration of surfactant. A study of the leachingof surfactants from the soil is important, as it is difficult to identify the reason for thereduction of concentration of pollutants in the soil: is it degradation or leaching? Theexperiments were carried out with a fine sandy soil in column tests and CaCO3 was added toincrease soil pH. The soil was treated twice with the bioremediation agent SR-100. The soilpH, the concentrations of anionic surfactant and petroleum hydrocarbons at the differentdepths of soil were determined. The microbial activity of soil fractions was evaluated byrespirometer. The concentration of surfactants was determined colorimetrically as MethyleneBlue active substances (MBAS). The concentration of anionic surfactants decreased in theupper layer of the columns, but it increased in the lower layers. It indicated the leaching ofthe anionic surfactants from soil during experiments of 60 days. The amounts of residualsurfactants were lower in the samples of polluted soil in comparison with unpolluted soil. Thesamples of lower soil fractions had higher microbial activity in comparison with upperfractions. Soil pH was measured as pHH20, pHKcl and pHcac12 instead of the pH of soilsolution, because soil was too dry. The pH of fine sandy soil was 5.8 and during theexperiment the value of pH increased in the lower layer of soil till pHH20 = 7.5.


1993 ◽  
Vol 39 (10) ◽  
pp. 922-931 ◽  
Author(s):  
Dilip K. Arora ◽  
Sushma Gupta

The chemotactic response of four common soil bacteria, Agrobacterium radiobacter, Bacillus subtilis, Pseudomonas fluorescens, and Xanthomonas malvacearum, was observed in natural soil to conidia of Cochliobolus sativus, chlamydospores of Fusarium oxysporum f.sp. ciceri, sclerotia of Macrophomina phaseolina, and oospores of Phytophthora drechsleri f.sp. cajani. All bacteria migrated through soil toward fungal spores. Chemical analysis of fungal exudates demonstrated the presence of various amino acids and sugars that served as chemoattractants. The effect of temperature, pH, soil water matric potential, and soil texture on bacterial chemotaxis toward fungal spores was also investigated. In general, the response of bacteria to different types of fungal spores was significantly greater (P = 0.05) at higher water matric potential (0 and −5 kPa) than at lower soil water potential (−10 and −20 kPa). The chemotactic response was greatest in sandy soil, followed by sandy loam and clay loam soil. High temperature (40 °C) was not favourable for bacterial chemotaxis. The chemotactic response decreased by 4 to 28 times when soil pH decreased from 7 to 5 or increased from 7 to 9. The relative concentration response of the exudate of fungal spores and the motility or chemotaxis of bacteria were assessed. A significant positive correlation (P = 0.05; r = 0.89–0.92) was recorded between motility and relative concentrations of exudate. The swimming speed and tumbling frequency of Pseudomonas fluorescens cells was observed at different pH values and temperatures. The swimming speed of bacteria increased with increasing temperature, but decreased with an increase in pH from 5 to 7. The tumbling frequency had a sharp peak at 30 °C and pH 7. Bacteria were able to stimulate the release of exudate from the fungal spores. The amount of exudation was also affected by temperature, pH, and soil texture. A positive significant correlation (P = 0.05; r = 0.79–0.85) was recorded between exudation and a progressive increase in temperature. The amount of exudation also increased with an increase in soil pH from 5 to 8, but further increases in pH decreased the rate of exudation. In general, fungal spores exuded the greatest amounts of carbon compounds in sandy soil, followed by sandy loam and clay loam soil. Exudation in sandy soil was often greatest in the presence of A. radiobacter cells, while the greatest exudation in sandy loam and clay loam soils was induced by B. subtilis cells.Key words: chemotaxis, chemoattractants, fungal spores, motility.


1983 ◽  
Vol 14 (6) ◽  
pp. 481-495 ◽  
Author(s):  
L. M. Shuman ◽  
F. C. Boswell ◽  
K. Ohki ◽  
M. B. Parker ◽  
D. O. Wilson
Keyword(s):  
Soil Ph ◽  

1978 ◽  
Vol 58 (1) ◽  
pp. 129-140
Author(s):  
J. M. DESCHENES ◽  
J. C. ST-PIERRE ◽  
L. BELZILE

Agronomic tests involving forage kale, silage corn, three cereals, three legumes and four grasses were performed in four ecological habitats. Differences in yield were found and three agronomic regions were determined. All species except wheat and clovers (red and white) performed very well in the middle and lower slopes of the appalachian highlands, characterized by the bent grass–red fescue association. Forage kale, corn and grasses gave good yields in the sandy soil region characterized by the poverty grass–mouse-eared hawkweed association whereas cereal and legume yields were low. In the lowlands dominated by red fescue, forage kale, cereals except wheat and grasses except bromegrass showed good performance whereas silage corn and legumes gave very poor yields. Within the county, forage kale gave the best yield and wheat the worst. In general, yield and persistence of legumes were poor in all regions but alfalfa performed fairly well in the middle and lower slopes of the highland. Grasses showed good adaptation and performance everywhere except bromegrass in the lowland region. Drainage, soil pH and natural fertility were the obvious limiting ecological factors responsible for yield differences among species and regions.


Author(s):  
N.A. Thomson

In a four year grazing trial with dairy cows the application of 5000 kg lime/ ha (applied in two applications of 2500 kg/ha in winter of the first two years) significantly increased annual pasture production in two of the four years and dairy production in one year. In three of the four years lime significantly increased pasture growth over summer/autumn with concurrent increases in milk production. In the last year of the trial lime had little effect on pasture growth but a relatively large increase in milkfat production resulted. A higher incidence of grass staggers was recorded on the limed farmlets in spring for each of the four years. In the second spring immediately following the second application of lime significant depressions in both pasture and plasma magnesium levels were recorded. By the third spring differences in plasma magnesium levels were negligible but small depressions in herbage magnesium resulting from lime continued to the end of the trial. Lime significantly raised soil pH, Ca and Mg levels but had no effect on either soil K or P. As pH levels of the unlimed paddocks were low (5.2-5.4) in each autumn and soil moisture levels were increased by liming, these factors may suggest possible causes for the seasonality of the pasture response to lime


Sign in / Sign up

Export Citation Format

Share Document