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 LIME AND GYPSUM APPLICATIONS ON SOIL CHEMICAL ATTRIBUTES AND INITIAL GROWTH OF EUCALYPTUS

FLORESTA ◽  
2018 ◽  
Vol 48 (4) ◽  
pp. 573 ◽  
Author(s):  
Camila Adaime Gabriel ◽  
Paulo Cezar Cassol ◽  
Marcia Aparecida Simonete ◽  
Letícia Moro ◽  
Priscylla Pfleger ◽  
...  
Keyword(s):  
Electrical Conductivity ◽  
Soil Ph ◽  
Soil Phosphorus ◽  
Dry Weight ◽  
Initial Growth ◽  
Soil Electrical Conductivity ◽  
Shoot Dry Weight ◽  
Eucalyptus Dunnii ◽  
Negative Effect ◽  
Chemical Attributes

Eucalyptus crops in Southern Brazil are generally conducted in acidic soils, thus their yield can be increased by lime and gypsum applications. The objective of this study was to evaluate the effect of lime and gypsum applications on soil chemical attributes and initial growth of Eucalyptus benthamii and Eucalyptus dunnii in a Humic Cambisol (Inceptisol). The experiment was conducted in a greenhouse, with seedlings of both species of eucalyptus grown in soil treated with different rates of lime (0, 3, 6, and 12 Mg ha-1), and gypsum (0, 6, 3, 12.6, and 25.2 Mg ha-1). At 90 days after application of the treatments, the soil chemical attributes and growth components of eucalyptus seedlings. The lime increased the production shoot dry weight, however, the response to gypsum was negative. The lime increased the soil pH, exchangeable calcium (Ca), base saturation (V %), and slightly the soil electrical conductivity, decreased the soil aluminium saturation (m %), and promoted little reduction in the exchangeable potassium (K) and magnesium (Mg) contents. The gypsum didn't alter the soil pH, but decreased the m%, increased soil phosphorus (P) contents, and expressively increased the electrical conductivity, which may have had a negative effect on the eucalyptus growth. In conclusion, the addition of limestone decreases the soil acidity and benefits the growth of eucalyptus seedlings. However, the addition of gypsum has no expressive effects upon those variables, but it can decrease the growth of seedlings when the rates are excessive.

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.

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.

RESPONSE OF A HYBRID POPLAR CLONE TO SOIL ACIDIFICATION AND LIMING

1985 ◽  
Vol 65 (4) ◽  
pp. 727-735 ◽  
Author(s):  
V. R. TIMMER
Keyword(s):  
Soil Ph ◽  
Aluminum Toxicity ◽  
Hybrid Poplar ◽  
Dry Weight ◽  
Fine Sand ◽  
Forest Tree ◽  
Maximum Height ◽  
Shoot Dry Weight ◽  
Wide Range ◽  
Poplar Cuttings

Unrooted hybrid poplar cuttings were grown in a greenhouse at varying soil pH. The soil was a loamy fine sand (pH 5.7) collected from an Ap horizon of a forest tree nursery. The pH was adjusted over a wide range by incorporating different rates of powdered lime or elemental sulfur. Lime additions failed to improve growth significantly over a 20-wk period, and excessive liming to pH 7.6 reduced shoot dry weight by 33%, probably because of decreased availability of micronutrients. Sulfur, acidifying the soil to pH 4.1, depressed growth as much as 76%. This growth inhibition was closely associated with increased Al in both foliage and soil as well as reduced foliar uptake of the other essential nutrients. Maximum height growth of clone DTAC-32 occurred between pH 6.0 and 7.0, which falls within the general guidelines for producing hardwood nursery stock. Key words: Populus, soil pH, aluminum toxicity, micronutrient deficiency

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 Improvement of Selected Soil Chemical Properties and Potassium Uptake by Mung Beans After Application of Liquid Organic Fertilizer in Ultisol

2018 ◽  
Vol 1 (1) ◽  
pp. 1-7
Author(s):  
Tristantia Anggita ◽  
Zainal Muktamar ◽  
Fahrurrozi Fahrurrozi
Keyword(s):  
Soil Ph ◽  
Mung Bean ◽  
Organic Fertilizer ◽  
Chemical Properties ◽  
Dry Weight ◽  
Soil Chemical Properties ◽  
K Uptake ◽  
Exchangeable K ◽  
Shoot Dry Weight ◽  
Animal Wastes

Recently, application of liquid organic fertilizer (LOF) in organic farming practices is of importance to prevent further soil degradation due to prolong and massive use of synthetic fertilizer. LOF provides faster plant nutrients than soil organic fertilizer. However, quality of LOF is substantially dependent on its sources. Animal wastes from rabbit, goat, and cattle are scarcely used as sources of LOF production. The study aimed to determine soil chemical improvement and potassium uptake by mung bean  as affected by LOF in Ultisol. The experiment was conducted at the Greenhouse Faculty of Agriculture, employing Completely Randomized Design with two factors. The first factor was animal wastes, consisting of goat, rabbit, and cattle wastes. The second factor was LOF concentration, consisting of 0%, 25%, 50%, 75%, and 100% LOF. LOF was prepared by mixing altogether animal feces, urine, soil, green biomass, EM-4 and fresh water to total volume of 10 l in a plastic container. LOF was decanted to the polybag every week starting at one week after planting for four weeks to a total volume of 750 ml per polybag. Variables observed included soil pH, total organic-C, exchangeable K, soil nitrate-N, K concentration in plant tissue, K-uptake, and shoot dry weight of sweet corn The result showed that application of LOF from rabbit waste had the highest increment of soil pH as compared to the other treatment. However, exchangeable K was observed highest at the treatment of LOF from goat waste. Sources of LOF from animal wastes did not have an effect on K-uptake by mung bean. In addition, application of LOF up to 100% was able to improve soil chemical properties as indicated by the increase in soil pH and exchangeable K. So did the concentration and uptake of K, as well as shoot dry weight. Fertilization with LOF has benefit to the improvement of soil chemical properties leading to better K uptake.

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. .

Effects of lime on the growth and nodulation of four grain legumes.

Soil Research ◽  
1982 ◽  
Vol 20 (3) ◽  
pp. 265 ◽  
Author(s):  
RS Jessop ◽  
J Mahoney
Keyword(s):  
Soil Ph ◽  
Shoot Growth ◽  
Root Nodules ◽  
Dry Weight ◽  
Grain Legumes ◽  
Ph Values ◽  
Field Peas ◽  
Root And Shoot Growth ◽  
Faba Beans ◽  
Top Dry Weight

Using an acid sand with differing proportions of added ground limestone, a range of soil pH levels was achieved from 5.4 to 9.2. Four winter grain legumes (field peas, faba beans, lupins and chickpeas) were grown for 8 weeks before being sampled for nodulation, dry matter and nitrogen production. Chickpeas appeared the least affected by the range of soil pH values and calcium levels in terms of root and shoot growth; all the legumes produced the greatest number of root nodules at pH 7 or 8. Top dry weight production in lupins was maximized at pH 6, and declined rapidly above pH 7; field peas, chickpeas and faba beans all showed maximum above-ground dry weights between pH 7 and 8.

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.

scholarly journals Variation of Cicer Germplasm to Manganese Toxicity Tolerance

2020 ◽  
Vol 11 ◽  
Author(s):  
Karthika Pradeep ◽  
Richard W. Bell ◽  
Wendy Vance
Keyword(s):  
Acid Tolerance ◽  
Dry Weight ◽  
Manganese Toxicity ◽  
Limiting Factor ◽  
Mn Toxicity ◽  
Shoot Dry Weight ◽  
Cicer Echinospermum ◽  
Wild Accessions ◽  
Low Ionic Strength ◽  
Mn Concentrations

After aluminum, manganese toxicity is the most limiting factor for crops grown in acidic soils worldwide. But overall, research on Mn toxicity is still limited. The poor acid tolerance of chickpea may be related to Mn toxicity, but there has been no previous screening of chickpea germplasm (nor in its wild Cicer relatives, Cicer reticulatum and Cicer echinospermum) for tolerance to Mn toxicity. A screening technique was developed for tolerance to Mn toxicity using three released cultivars of chickpea (Cicer arietinum L), Ambar, PBA HatTrick, and PBA Striker; one accession each of C. reticulatum and C. echinospermum; and lupin (Lupinus angustifolius) as a Mn-tolerant check, with eight Mn concentrations of 2, 25, 50, 100, 150, 200, 250, and 500 μM Mn as MnSO4 in a low-ionic-strength nutrient solution. The plants were harvested at 14 and 28 days after Mn treatments. The nutrient uptake in shoots (young, old leaves, and the rest of the shoot) and roots was investigated. The best discrimination between tolerant and intolerant Cicer genotypes based on relative shoot dry weight, root dry weight, total root length, and scoring of toxicity symptoms was achieved at 150 μM Mn after 14 days of growth in Mn solution. Among the chickpea cultivars, the greater relative plant growth (both shoot and root) of Ambar and PBA Striker at 100–200 μM Mn contrasted with that of PBA HatTrick, while the C. echinospermum accession was more tolerant to Mn toxicity than C. reticulatum. Manganese tolerance in both domestic cultivars and wild accessions was associated with internal tolerance to excess Mn following greater uptake of Mn and translocation of Mn from roots to shoots.

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