The effect of soil pH on potassium intensity and release of non-exchangeable potassium to ryegrass

1970 ◽  
Vol 75 (3) ◽  
pp. 571-576 ◽  
Author(s):  
A. Islam ◽  
J. Bolton
Keyword(s):  
Soil Ph ◽  
Sandy Soil ◽  
Acid Soils ◽  
The Other ◽  
Exchangeable Potassium ◽  
Air Drying ◽  
Ph Values ◽  
Small Constant ◽  
Activity Ratios ◽  
Exchangeable Form

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.

scholarly journals Effect of black peat, pH and Mg on growth of heather on sandy soil.

1986 ◽  
Vol 34 (1) ◽  
pp. 103-106
Author(s):  
H. Niers ◽  
J. van der Boon
Keyword(s):  
Soil Ph ◽  
Sandy Soil ◽  
Calluna Vulgaris ◽  
Field Trials ◽  
The Other ◽  
High Ph ◽  
Visual Rating ◽  
Top Soil ◽  
Negative Effect ◽  
Mg Content

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)

Soil pH and aluminium and their spatial variation in Western Australian acidic soils

1990 ◽  
Vol 30 (5) ◽  
pp. 637 ◽  
Author(s):  
PJ Dolling ◽  
WM Porter ◽  
AD Robson
Keyword(s):  
Spatial Variation ◽  
Soil Ph ◽  
Surface Soil ◽  
Acid Soils ◽  
Poor Correlation ◽  
Ph Values ◽  
Coefficients Of Variation ◽  
Subsurface Soil ◽  
The Relationship ◽  
Surface Soil Ph

Thirty-eight sites on acid soils (pH<5.5, 1:5 in water) in the medium rainfall region of Western Australia were sampled to examine spatial variation in soil pH and 0.01 mol/L CaCl2-extractable aluminium. We also examined the relationship between (i) the A1 and A2 horizon soil pH, (ii) the A1 and A2 horizon extractable aluminium, (iii) surface and subsurface soil pH and (iv) surface soil and subsurface soil-extractable Al. Soil at each site generally had a light-textured layer overlying a clay layer at varying depths (30-70 cm) and was classified as either Dy 5.21 or Dy 5.41 (Northcote 1979). Over 80% of the sites had surface soil pH values 4.8 or lower and extractable aluminium concentrations 2 �g/g or higher. There was a very poor correlation (r2 = 0.21) between the A1 horizon soil aluminium extracted in 0.01 mol/L CaCl2 and the pH measured in 0.01 mol/L CaCl2 over 1 ha sites. The relationship was slightly improved in the A2 horizon (r2 = 0.49). The coefficients of variation of soil pH varied from 1.2 to 5.1%, while the coefficients of variation for CaCl2-extractable aluminium varied from 10 to 50%. At many of the sites, low pH values and high aluminium concentrations extended down to 35-45 cm. At the B horizon the pH values generally increased and the aluminium concentrations decreased. The surface soil pH and extractable aluminium were not good indicators (r2 = 0.09-0.60) of the subsurface soil pH and extractable aluminium.

The pH of Puerto Rican Soils Used for Principal Crops

1969 ◽  
Vol 46 (2) ◽  
pp. 107-119
Author(s):  
George Samuels
Keyword(s):  
Puerto Rico ◽  
Puerto Rican ◽  
Soil Ph ◽  
Acid Soils ◽  
Soil Series ◽  
Root Crop ◽  
Ph Values ◽  
Ph Range ◽  
The Relationship ◽  
Acid Range

The pH values of the soils of Puerto Rico were determined with the following results: 1. About 80 percent of the soils were acid (below pH 7) and 50 percent were below pH 6, which was acid enough to require liming. 2. Most of the soils planted to bananas were pH 6 and above. 3. The pH range for brushland was wide, extending from acid to alkaline. 4. Eighty percent of the soils of the coconut plantations were above pH 6. 5. Coffee soils, in general, were acid, with 63 percent below pH 6, of which 49 percent were in the range pH 5.0 to 5.9 and 13 percent in the very acid range of pH 4.0 to 4.9. 6. The pH of soils planted to corn varied widely. 7. The small cotton acreage had a pH range of 5.0 to 5.9. 8. The soils planted to grapefruit had 57 percent of their acreage at pH 4.0 to 4.9 and 29 percent in the range pH 5.0 to 5.9. 9. The natural pastures had 75 percent of their soil at pH below 6, whereas improved and rotational pastures had only 39 percent below pH 6. 10. Pineapples were planted in acid soils, 75 percent of which were below pH 6. 11. The majority, 68 percent, of the plantains were grown in acid soils below pH 6. 12. Root-crop soils had a systematic distribution throughout the range of pH from below 4 to above 8. 13. Most soils used for soilage (cut grass) had a pH above 6. 14. Eighty-one percent of the sugarcane acreage was found to be in the range of pH 5 to 8. About 36 percent of the cane acreage was below pH 5.5 and in need of liming. 15. Tobacco was grown primarily on acid soils, with 61 percent of its acreage on those below pH 6. 16. No vegetables were found in soils with a pH below 5, and 50 percent were planted in soils with a pH above 6. 17. The pH range for woodland soil was distributed rather evenly from a pH 5 to 7.9. 18. The average pH and range of pH of the soils of Puerto Rico are presented, by soil series, and several examples are given of the relationship between soil pH and soil series.

scholarly journals SOIL pH MEASUREMENT AND ITS APPLICATION TO ORGANIC SOILS

1977 ◽  
Vol 57 (1) ◽  
pp. 55-64 ◽  
Author(s):  
WM. van LIEROP ◽  
A. F. MacKENZIE
Keyword(s):  
Ionic Strength ◽  
Soil Ph ◽  
Growing Season ◽  
Application Rate ◽  
The Other ◽  
Organic Soils ◽  
Significant Treatment ◽  
Hydrogen Saturation ◽  
Ph Values ◽  
Exchangeable Hydrogen

The average soil pH of 10 organic soils was significantly influenced by drying and the salt concentration of the suspending media. Accordingly, mean soil pH of field-moist and oven-dried soils was pH 5.0 and 4.5, 4.1 and 3.9, and 3.8 and 3.6 for soils suspended in water, 0.015 M CaCl2 and 1 M KCl. A significant treatment–soil interaction indicated that the soils responded differently to the treatments. No junction potentials were found when the ionic strength of the solution was 0.01 M CaCl2 equivalent or greater. Milli-equivalents exchangeable hydrogen (−0.984**), percent hydrogen saturation (−0.966**) milli-equivalents extractable bases (0.937**) and percent base saturation (0.957**) were more closely correlated with 1 M KCl pH values than with values in the other media. Liming influenced soil pH significantly on all field sites and within 8 h after application on two field sites. The influence of liming on soil pH tended to diminish the year after applications were made. Measured soil pH variability among treatments and replicates at various sampling dates ranged up to 1 pH unit during the growing season. However, it was about 0.2 pH unit on the control treatments with undetectable quantities of residual limestone. The quantity of reacted limestone was established at 25 and 40%, between 23 May and 31 July, on two sites (J.I.V. and S.B.). The reacted limestone was found to be proportional to the application rate.

scholarly journals Some negative chemical properties of acid soils

2005 ◽  
Vol 70 (5) ◽  
pp. 765-774 ◽  
Author(s):  
Miodrag Jakovljevic ◽  
Mirjana Kresovic ◽  
Srdjan Blagojevic ◽  
Svetlana Antic-Mladenovic
Keyword(s):  
Soil Properties ◽  
Soil Ph ◽  
Acid Soil ◽  
Chemical Properties ◽  
Acid Soils ◽  
Strong Inhibition ◽  
Brown Forest Soil ◽  
Ph Values ◽  
Inhibition Of Nitrification ◽  
Influence Of Ph

Some important chemical properties of various samples of two types of acid soil from Western Serbia (pseudogley and brown forest) are presented in this paper. Mobile Al was found in elevated and toxic quantities (10?30 mg/100 g) in the more acid samples of pseudogley soil. All samples of brown forest soil were very acid and the quantities of mobile Al were in the range from 12.8 to 90.0 mg/100 g. In a selected number of pseudogley soils, the influence of pH and other soil properties on the mineralization and nitrification processes was investigated. Strong inhibition of nitrification at low soil pH was found to be related to high quantities of mobile Al. At pH values less than 4.0 (in 1 M KCl), processes of chemical nitrification and denitrification of applied nitrites were registered in the pseudogley soils. .

Accumulation and distribution of toxic and potentially toxic elements in potato on different types of soil

2020 ◽  
Author(s):  
Jelena Popović-Djordjević ◽  
Zoran Broćić ◽  
Mirjana Kresović ◽  
Jelena Mutić
Keyword(s):  
Trace Elements ◽  
Soil Ph ◽  
Toxic Elements ◽  
Potato Production ◽  
Soil Samples ◽  
The Other ◽  
Emission Spectrometry ◽  
The Core ◽  
Ph Values ◽  
Other Hand

&lt;p&gt;Potato is currently the third most significant crop culture in the world, with the production of over 388 million tons in 2016. This crop is present on the tables of Serbian consumers throughout the year because of the tradition and its affordable price. Serbia has relatively good climatic conditions for potato production, which are defined by the temperature regime and the amount and frequency of precipitation. The nutritive value of the potato is mainly attributed to the chemical composition of the tuber. The element composition of tubers depends on many factors, such as: genotype, developmental phase of the plant, agroecological conditions, chemical properties of soil, fertilization and irrigation. On the other hand, geochemical origin of trace elements in the soil, the intensive agriculture production, use of contaminated soil and irrigation water may increase their toxic levels in tubers.&lt;/p&gt;&lt;p&gt;&amp;#160;Potato tubers of five varieties were produced on commercial farms at two locations in Western Serbia (Gu&amp;#269;a and Sjenica), with favorable agroecological conditions for potato production. Tuber samples of studied varieties from each location were collected at the end of growing seasons at the stage of physiological maturity. Soil samples were collected from several sites at each production location at the depth of 0&amp;#8211;30 cm. Basic agrochemical properties of the soil samples were determined. Content of toxic (As, Cd, Pb) and potentially toxic (Al, Ba, Ni, V) elements in fresh tubers (peel and core) and soil samples was established by inductively coupled plasma&amp;#8211;optical emission spectrometry (ICP&amp;#8211;OES). Bioaccumulation factor (BAF) of each studied element, as the ratio between its content in the peel and in the core of the tuber and the soil, was calculated.&lt;/p&gt;&lt;p&gt;&amp;#160;According to pH values, 4.77 and 6.80, soils were clasified as very acidic (Gu&amp;#269;a location) and slightly acidic (Sjenica location), respectively. Content of studied trace elements in soils, with the exception of Ni, was within the allowable limits. Tuber peel of all studied varieties grown on both soil types was characterized with the higher content of Cd, Al, Ba and Ni, compared to the relevant core. Consenquently, the higher values of BAF were observed in the peel of tubers. Average values of BAF for the studied elements in the peel for both soil pH values 4.77 and 6.80 (Gu&amp;#269;a and Sjenica, respectively) were in the following order: Cd&gt;Ba&gt;Pb&gt;As&gt;Ni&gt;Al=V. On the other hand, average BAF values for the core of the tuber samples were in a slightly different order, depending on the soil pH; Cd&gt;Pb&gt;As&gt;Ba&gt;Ni&gt;Al=V (pH 4.77) and Cd&gt;Pb&gt;As&gt;Ba=Ni&gt;V (pH 6.80). The highest/lowest BAFs were calculated for Cd (0.339) in the peel and Al (0.0002) in the core, respectively. Content of As and Cd did not exeed the maximum allowed concentrations set by the national and European Union regulations, but it should be pointed out that Cd content was close to the upper limit. Also, it was noticed that the content of Pb exceeded the safe limit set for these elements according to both regulations.&lt;/p&gt;&lt;p&gt;Keywords: potato tuber, soil, toxic elements, ICP&lt;/p&gt;&lt;p&gt;Acknowledgement: This work was supported by the Ministry of Education, Science and Technological Development of the Republic of Serbia (Research grant No. 46009).&lt;/p&gt;

WATER-SOLUBLE AND EXCHANGEABLE ALUMINUM IN ACID SOILS AS AFFECTED BY LIMING AND FERTILIZATION

1967 ◽  
Vol 47 (3) ◽  
pp. 203-210 ◽  
Author(s):  
L. B. MacLeod ◽  
L. P. Jackson
Keyword(s):  
Soil Ph ◽  
Surface Soil ◽  
Acid Soils ◽  
Water Soluble ◽  
Ph Values ◽  
Exchangeable Al ◽  
Exchangeable Aluminum ◽  
High Fertilization ◽  
Surface Soil Ph ◽  
Representative Samples

The concentration of water-soluble and exchangeable aluminum was determined in the 0–15-, 15–23-, 23–30- and 30–45-cm depths of a Podzol limed to provide surface soil pH values ranging from 4.5 to 7.2. Both soluble and exchangeable Al decreased with increasing soil pH. Soluble Al ranged from 5.7 ppm at pH 4.4 with high fertilization to 0.3 ppm at pH 6.5 with similar fertilization. Increasing the rate of fertilization at pH 4.5 raised the soluble Al from 2.6 to 5.7 ppm. Fertilization still doubled the soluble Al in soil at pH 5.1 but had little effect as the pH was raised further to 5.8 and 6.5. Soluble Al in the subsoil samples was less than in surface soil samples at the same pH, while with exchangeable Al, the concentration was greater in the subsoil than in the surface soil samples.There was not a direct relationship between pH and soluble Al, although the highest soluble Al concentrations occurred at lowest soil pH levels. Analyses of 30 representative samples of surface soil taken from farmers' fields showed that the soluble Al concentration at pH 4.0 ranged from 3.5 to 4.8 ppm, while at a pH of 5.0 it ranged from 0.2 to 2.8 ppm. The concentrations of soluble Al in many of these soils exceeded the levels previously shown by nutrient solution experiments to severely restrict growth of legumes and some varieties of barley.

Emergence of Medicago tribuloides on moderately acid soils

1965 ◽  
Vol 16 (3) ◽  
pp. 311 ◽  
Author(s):  
CR Kleinig
Keyword(s):  
Soil Ph ◽  
Ph Effect ◽  
Acid Soils ◽  
Inorganic Materials ◽  
Soil Organisms ◽  
Seedling Mortality ◽  
Adverse Conditions ◽  
Ph Values ◽  
High Soil Moisture ◽  
Viable Seeds

Field establishment of Medicago tribuloides Desr. on moderately acid, light textured soils varied from 98% to less than 10% of untreated viable seeds sown. Seed and seedling mortality occurred mainly in the pre-emergence stage. Where emergence was poor, under conditions of low temperature or high soil moisture, or both, considerable improvement resulted from using a seed fungicide or a soil fumigant, or coating seeds with alkaline inorganic materials, of which calcium carbonate was the most effective. Under adverse conditions of temperature and rainfall, improved emergence occurred at higher soil pH values. The results indicate that pathogenic soil organisms caused pre-emergence seed and seedling mortality, and that temperature, rainfall, soil pH, and seed coating (through its pH effect) influenced pathogen activity or the susceptibility of the seedling to pathogenic attack.

Differential tolerance of genotypes of Medicago truncatula to low pH

1992 ◽  
Vol 43 (3) ◽  
pp. 731 ◽  
Author(s):  
M Bounejmate ◽  
AD Robson
Keyword(s):  
Medicago Truncatula ◽  
Soil Ph ◽  
Acid Soils ◽  
Acid Tolerance ◽  
Dry Weight ◽  
Low Ph ◽  
Commercial Cultivar ◽  
Ph Values ◽  
Shoot Dry Weight

Growth and nodulation of five Moroccan ecotypes of Medicago truncatula Gaertn. Collected from soils of different pH, Medicago truncatula cv. Cyprus and Medicago murex Willd. cv. Zodiac, were compared in soil and solution at different pH values. The seven genotypes tested varied greatly in their ability to grow and nodulate on acid soils. Increasing soil pH from 4.5 to 5.4 increased the shoot dry weight of Cyprus and three M. truncatula ecotypes but not Zodiac and two M. truncatula ecotypes. Cultivar Cyprus, with a shoot dry weight at pH 4.5 only 58% of that at pH 5.4, was the most affected by acidity. Nodulation was the most sensitive step as nodule numbers decreased with increasing acidity for sensitive genotypes. Several genotypes were more able to nodulate at low pH than the commercial cultivar Cyprus. Acid tolerance was not restricted to genotypes occurring naturally in acid soils.

scholarly journals Effect of the Soil pH on the Alkaloid Content ofLupinus angustifolius

2012 ◽  
Vol 2012 ◽  
pp. 1-5 ◽  
Author(s):  
Gisela Jansen ◽  
Hans-Ulrich Jürgens ◽  
Edgar Schliephake ◽  
Frank Ordon
Keyword(s):  
Soil Ph ◽  
Field Experiments ◽  
Calcareous Soils ◽  
Acid Soils ◽  
Field Studies ◽  
Lupinus Angustifolius ◽  
Alkaloid Content ◽  
Genotypic Differences ◽  
Ph Values ◽  
Growing Seasons

Field studies were conducted in growing seasons 2004, 2005, and 2010 to investigate the effect of different soil pH values on the alkaloid content in seeds ofLupinus angustifolius. Two-year experiments with eleven cultivars were carried out in acid soils with an average ofpH=5.8(Mecklenburg-Western Pomerania) and on calcareous soils with an average pH of 7.1 (Bavaria), respectively. In addition, in 2010, eight cultivars were grown in field experiments in soils with pH values varying betweenpH=5.3andpH=6.7. In all experiments conducted on soils with a higher pH (pH=6.7andpH=7.1), a significantly lower alkaloid content was detected in allLupinus angustifoliuscultivars than on soils with a lower pH (pH=5.3andpH=5.8). Results clearly show that the alkaloid content is significantly influenced by the soil pH but genotypic differences regarding the reaction to different pH values in the soil were observed.

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