EFFETS DES DOSES DE MANGANESE, D’ALUMINIUM, DES REGIMES HYDRIQUES ET DU pH DES SOLS SUR LES RENDEMENTS DE LUZERNE ET SUR L’ASSIMILABILITE DU MANGANESE ET DE L’ALUMINIUM

1985 ◽  
Vol 65 (2) ◽  
pp. 269-282 ◽  
Author(s):  
J. L. DIONNE ◽  
A. R. PESANT
Keyword(s):  
Soil Moisture ◽  
Soil Ph ◽  
Acid Soils ◽  
Field Capacity ◽  
High Concentration ◽  
Saturation Point ◽  
High Soil Moisture ◽  
A Value ◽  
Moisture Regimes ◽  
High Level

Alfalfa (Medicago sativa L. ’Saranac’) was grown on Ste. Rosalie clay, Greensboro loam and St. Jude sand adjusted to about pH 5.0, 6.5 and 7.5 in a greenhouse experiment, to determine the changes in response of alfalfa to aluminum and manganese resulting from variations in soil pH and soil moisture. Rates of Mn were equivalent to 0 and 200 kg∙ha−1 and rates of Al were 0, and 100 kg∙ha−1. Three soil moisture regimes were used: (1) Optimum with soil moisture between field capacity (FC) and 70% of this value. (2) Wet: with soil moisture between saturation point (SP) and FC. (3) Very wet: with soil moisture between saturation point and a value half way between SP and FC. Manganese applied on acid soils (pH 5.2) under optimum soil moisture regimes decreased alfalfa yields by 3% only, compared to a 62% decrease in alfalfa yields by Mn applied on acid soils of the two high soil moisture regimes. This was due to a high level of Mn in alfalfa on the wet acid soils. A large quantity of aluminum was also found in alfalfa grown in acid soils along with a high concentration of "extractable" aluminum. This resulted in a 54% reduction of alfalfa yields. Content of Al and Mn in alfalfa top and in soils was decreased sharply by liming soils at pH of 6.5 or 7.5. On soils limed to a pH of about 7.0 alfalfa survived at high levels of Mn and Al such as frequently encountered in some acid and very wet soils. Key words: Soil Mn, soil Al, soil pH, soil moisture, alfalfa

EFFETS DES REGIMES HYDRIQUES ET DES pH DU SOL SUR LA REPONSE AU MOLYBDENE DE LA LUZERNE

1986 ◽  
Vol 66 (3) ◽  
pp. 421-435
Author(s):  
J. L. DIONNE ◽  
A. R. PESANT
Keyword(s):  
Soil Moisture ◽  
Key Words ◽  
Soil Ph ◽  
Soil Type ◽  
Sandy Loam ◽  
Acid Soils ◽  
Combined Effect ◽  
Moisture Regimes ◽  
Mo Content

The objectives of this study were to determine the changes in response of alfalfa (cv. Saranac) to molydbenum applications from variations in soil pH and soil moisture. To achieve these ends the test crop was grown on three replicates of the following treatments: Three soils (Ste Rosalie clay, Greensboro loam and Danby sandy loam) adjusted to approximately pH 5.0, 6.5, and 7.5 fertilized at 0.0, 0.1, 0.2 and 0.3 mg Mo kg−1 of soil and maintained at three moisture levels: dry, optimal and saturated. Yields were not affected by molybdenum applications regardless of soil type, soil pH or soil moisture regimes. Mo content of alfalfa increased linearly with rates of Mo from 0.2 ppm to 23 ppm Mo. Liming soil to pH 7.2 produced the same increase of Mo content in alfalfa as applying Mo at the rate of 0.2 mg kg−1 to acid soils. Mo content of alfalfa was also slightly increased by soil moisture. A Mo content of 20 ppm or more was obtained as a result of the combined effect of molybdenum application, liming and soil moisture regimes. The exchangeable Mo content found in soils after the experiment increased with rate of Mo but decreased with increasing soil pH. The uptake of molybdenum was increased so much by liming that the Mo left in soil after cropping was decreased as soil pH increased. Key words: Mo content of soil, Mo content of alfalfa, soil pH, soil moisture, alfalfa

Quality and morphological characteristics of alfalfa as affected by soil moisture, pH and phosphorus fertilization

1992 ◽  
Vol 72 (1) ◽  
pp. 147-162 ◽  
Author(s):  
Hélène V. Petit ◽  
A. R. Pesant ◽  
G. M. Barnett ◽  
W. N. Mason ◽  
J. L. Dionne
Keyword(s):  
Soil Moisture ◽  
Soil Ph ◽  
Plant Morphology ◽  
Field Capacity ◽  
Phosphorus Fertilization ◽  
Moisture Regime ◽  
Available Water ◽  
Soil Moisture Regime ◽  
Temperature Regimes ◽  
Moisture Regimes

Alfalfa (Medicago sativa L. ’Saranac’) was grown in a greenhouse on Ste-Rosalie clay and Danby gravelly sandy loam to determine the effects of phosphorus fertilization, air temperature, soil moisture regime and soil pH on chemical composition and plant morphology. The following treatments were applied in factorial combination: three moisture regimes (1, semi-dry, with soil moisture between field capacity or 100% of available water and wilting point or 0% of available water; 2, optimal, between field capacity and 70% of available water; 3, wet, between saturation point and field capacity), three rates of phosphorus in the form of disodium phosphate (0, 12.5 and 25.0 P kg−1 of dry soil) and three soil pH levels (natural, near 5.4, 6.5 and 7.5). Half the alfalfa was grown in a warm greenhouse section with a minimum daytime temperature of 25 °C and 19 °C at night and the other half was grown in a cool section with a daytime minimum of 15 °C and 9 °C at night. Quality of alfalfa was generally improved by water deficit as shown by decreased concentrations of acid detergent fiber (ADF) and acid detergent lignin (ADL) and increased concentrations of crude protein (CP). Cold temperatures decreased ADF content which indicates that quality of alfalfa grown under cold compared to warm temperature regimes is better. Phosphorus fertilization seemed to have more effects on plant morphology and quality under cold than warm temperature regimes. In general, concentrations of CP, ADF and ADL, stem length, leaf area and the number of stems increased in parallel with soil pH. The data indicate that low temperature and low soil moisture regimes were generally associated with higher quality alfalfa than were high temperature and wet soil moisture regimes.Key words: Alfalfa, soil moisture regime, air temperature, phosphorus fertilization, soil pH

EFFETS DU pH ET DES REGIMES HYDRIQUES DES SOLS SUR LES RENDEMENTS ET LA TENEUR EN Mn DE LA LUZERNE ET DU LOTIER CULTIVES EN SERRE

1976 ◽  
Vol 56 (4) ◽  
pp. 919-928 ◽  
Author(s):  
J. L. DIONNE ◽  
A. R. PESANT
Keyword(s):  
Soil Moisture ◽  
Soil Ph ◽  
Acid Soil ◽  
Manganese Content ◽  
Field Capacity ◽  
Soil Conditions ◽  
Birdsfoot Trefoil ◽  
Moisture Regime ◽  
Soil Moisture Regime ◽  
Moisture Regimes

Alfalfa (Medicago sativa L.) and birdsfoot trefoil (Lotus corniculatus L.) were grown under greenhouse conditions, on Ste-Rosalie clay and St-Jude sand adjusted at pH of 5.0, 6.5 and 7.5, in order to determine the effect of soil pH and soil moisture regimes on the yields of the two legumes. Three soil moisture regimes were used: (1) humid (H1), with soil moisture between saturation point and field capacity; (2) optimum (H2), with soil moisture between field capacity and 70% of this value; (3) dry (H3), with soil moisture between 50% of field capacity and wilting point. Under the dry soil moisture regime (H3), birdsfoot trefoil behaved in the same way as did alfalfa. Their drought resistance decreased as the soil pH increased. Dry matter yields were reduced by 61.5% when soils were limed at the pH of 7.5. Under the humid soil moisture regime (H1), the productivity of alfalfa decreased much more than that of birdsfoot trefoil. The effect of excess soil moisture on alfalfa was mostly observed on the unlimed soils. Under these wet and acid soil conditions, alfalfa was intoxicated and suffocated due to high exchangeable manganese content and poor soil aeration. Liming soils to the pH of 7.5 decreased exchangeable Mn in soils to a non-toxic level and alfalfa could then grow well enough to transpire off the excess of soil water. Birdsfoot trefoil was much less influenced by soil acidity and poor drainage than alfalfa was.

EFFETS DES DOSES DE BORE, DES REGIMES HYDRIQUES ET DU pH DES SOLS SUR LES RENDEMENTS DE LA LUZERNE ET DU LOTIER ET SUR L’ASSIMILABILITE DU BORE

1978 ◽  
Vol 58 (3) ◽  
pp. 369-379 ◽  
Author(s):  
J. L. DIONNE ◽  
A. R. PESANT
Keyword(s):  
Soil Moisture ◽  
Soil Ph ◽  
Field Capacity ◽  
Soil Conditions ◽  
Birdsfoot Trefoil ◽  
Moisture Regime ◽  
Yield Increase ◽  
Soil Moisture Regime ◽  
Moisture Regimes ◽  
Wilting Point

Alfalfa (Medicago sativa L. cv. Vernal) and birdsfoot trefoil (Lotus corniculatus L. cv. Leo) were grown under greenhouse conditions in order to determine changes in boron response and availability following variations in soil pH and soil moisture regimes. Three rates of boron applications were selected: 0, 1.5, and 3.0 ppm of B. Soil pH was adjusted to 5.0, 6.5 and 7.5, respectively. The soil moisture regimes were fixed as following: (1) very dry (H1) with soil moisture between 50% of field capacity and wilting point, (2) dry (H2), with soil moisture between field capacity and wilting point. (3) optimum (H3), with soil moisture between field capacity and 70% of this value. Boron fertilization was more useful to alfalfa than to birdsfoot trefoil. Optimum rate was found to be 1.5 ppm of B. On Ste-Rosalie clay, the yield increase due to boron was 22% on soils under the dry regime (H2) but was almost non-existant at the very dry (H1) and optimum water regime (H3). Boron application on Greensboro loam was more efficient on soils undergoing dry (H2) and very dry soil moisture regime (H1) than on soils where moisture conditions were optimum (H3). Dry matter yields were increased by a factor of 10 under dry (H2) and very dry (H1) soil moisture regimes compared to a factor of 4 under optimum soil moisture regime (H3). Under acid soil conditions, no yield increase was obtained following boron applications. Boron availability and response of the two legumes to B was also decreased by overliming soils to pH 7.4. The cyclic drought periods that happened under dry (H2) and very dry (H1) soil moisture regime produced similar effects. Boron availability and efficiency as plant nutrient was greatly reduced, if not annihilated, by the combined effect of repeated drought cycles and by either excessive soil acidity or overliming.

scholarly journals Influence of pH and Matric Potential on Germination of Cephalosporium gramineum Conidia

Plant Disease ◽  
1998 ◽  
Vol 82 (9) ◽  
pp. 975-978 ◽  
Author(s):  
Cynthia A. Blank ◽  
Timothy D. Murray
Keyword(s):  
Soil Moisture ◽  
Soil Ph ◽  
Significant Influence ◽  
Phosphate Buffer ◽  
Mineral Salts ◽  
Matric Potential ◽  
High Soil Moisture ◽  
Soil Fungistasis ◽  
Cephalosporium Gramineum ◽  
Influence Of Ph

Germination of Cephalosporium gramineum conidia in soil was up to twofold greater at -0.064 MPa than at -0.037 and -0.007 MPa when incubated at 5°C for 2 days. Soil pH from 4.7 to 7.5 did not have a significant influence on germination of conidia and the interaction between soil pH and matric potential on germination was not significant. Soil fungistasis, which was previously observed for conidia of C. gramineum, was not observed in these studies. Germination of conidia on mineral salts agar containing phosphate buffer was significantly less at pH 4.5 than at 5.5, 6.5, or 7.5 at 5°C in one of two experiments; however, pH had no influence on germination at 10 or 20°C in two experiments. Although Cephalosporium stripe is more severe under conditions of high soil moisture and low soil pH, increased germination of conidia in response to these factors does not explain the observed increase in disease.

MICROORGANISMS IN THE ROOT ZONE IN RELATION TO SOIL MOISTURE

1965 ◽  
Vol 11 (3) ◽  
pp. 483-489 ◽  
Author(s):  
E. A. Peterson ◽  
J. W. Rouatt ◽  
H. Katznelson
Keyword(s):  
Soil Moisture ◽  
Soil Moisture Content ◽  
Root Colonization ◽  
Microbial Population ◽  
Root Zone ◽  
Root Surface ◽  
High Soil Moisture ◽  
High Soil ◽  
High Level ◽  
Taxonomic Studies

The influence of soil moisture on the microbial population of rhizosphere soil and of the root surface (rhizoplane) of wheat was studied under controlled conditions. Fertile soil adjusted to 30%, 60%, and 90% of its moisture-holding capacity was used. Bacterial counts and numbers of specific "physiological groups" of bacteria all increased in the rhizosphere and the rhizoplane as soil moisture decreased. Taxonomic studies of the bacteria isolated from the rhizoplane showed a marked preponderance of species of Pseudomonas under conditions of low and intermediate soil moisture content. On the other hand species of Arthrobacter, Bacillus, and Cytophaga dominated the population at high soil moisture. Although the distribution of fungi on the roots was very similar for the low and intermediate moisture levels, there was some restriction of colonization at the high level. Species of Mortierella, Rhizopus, Chaetomium, Curvularia, and Helminthosporium were not represented among isolates from roots at high soil moisture and the relative incidence of species of Fusarium and Phoma decreased. However, high soil moisture favored root colonization by species of Rhizoctonia and sterile dark fungi.

scholarly journals Influence of different liming material on soil pH and spring barley yield under different soil moisture conditions

2020 ◽  
Vol 27 (3) ◽  
Author(s):  
Donata Drapanauskaitė ◽  
Kristina Bunevičienė ◽  
Romas Mažeika
Keyword(s):  
Soil Moisture ◽  
Chemical Composition ◽  
Soil Ph ◽  
Spring Barley ◽  
Acid Soils ◽  
Nutrient Content ◽  
Magnesium Content ◽  
Liming Material ◽  
Agrochemical Properties ◽  
Moisture Conditions

Liming of acid soils is one of the most effective and multipurpose ways to improve soil properties. Liming changes the agrochemical properties, nutrient content and uptake. The aim of the research was to evaluate the influence of different liming materials on soil pH and spring barley yield under different soil moisture conditions. A vegetation experiment was performed until full yield formation under two different soil moisture conditions: optimum 17–20% and excess 28–31%. Liming materials of different physical forms and chemical composition were used in the experiment: ground, crushed and granulated liming materials, which differed in their chemical composition. Ground liming material had the highest neutralizing value (52.2 ± 0.40%) and reactivity (99.5 ± 0.18%), and crushed liming material had the lowest reactivity (10.0 ± 0.23%) and the highest (10.33 ± 0.148) magnesium content. Liming with ground liming material was the most effective and fastest way to neutralize soil acidity. It increased the soil pH from 4.44 ± 0.191 to 6.17 ± 0.042 under optimum moisture conditions and from 4.46 ± 0.156 to 6.76 ± 0.537 under excess moisture conditions after 4 weeks of liming. When spring barley was grown to full yield, a significant increase in yield in both years was found by liming with granulated liming material ø 2–5 mm in both soil moisture conditions, and the highest mass of 1,000th grain was obtained in the treatments limed with granulated liming material with potassium additive.

The Influence of Soil Moisture on the Foliar Activity of Diclofop

Weed Science ◽  
1980 ◽  
Vol 28 (5) ◽  
pp. 534-539 ◽  
Author(s):  
W. A. Dortenzio ◽  
R. F. Norris
Keyword(s):  
Soil Moisture ◽  
Near Field ◽  
Field Capacity ◽  
Herbicide Application ◽  
Wild Oats ◽  
High Soil Moisture ◽  
Herbicide Activity ◽  
Moisture Conditions ◽  
Soil Moisture Status ◽  
Wilting Point

Loss in activity of foliar-applied methyl ester of diclofop {2-[4-(2,4-dichlorophenoxy)phenoxy] propanoic acid} occurred under low soil moisture conditions. A loss in control of yellow foxtail [Setaria lutescens(Weigel) Hubb.], wild oats (Avena fatuaL.), little-seed canarygrass (Phalaris minorRetz.), and barnyardgrass [Echinochloa crus-galli(L.) Beauv.], was observed under greenhouse and growth chamber conditions. When soil was maintained at 2 to 3% above wilting point as compared to near field capacity, herbicide activity was decreased by 15 to 50%. High soil moisture (at or above 67% of field capacity) for at least 2 to 4 days following treatment was needed to achieve maximum effectiveness of the herbicide. Daily furrow irrigations for a period of 10 days following treatment of barnyardgrass in the field resulted in highest activity as compared to that under single irrigation regimes within the 10-day period. The effect of low soil moisture was minimized by increased rates of herbicide application. Hoe-29152 {methyl-2-[4-(4-trifluoromethylphenoxy)phenoxy] propanoate} showed similar losses in activity associated with low soil moisture. No consistent changes in uptake or translocation of14C-labeled diclofop could be detected in association with altered soil moisture status.

scholarly journals Effect of Hydropriming and soil moisture regimes on yield and yield components of maize (Zea mays L.)

2015 ◽  
Vol 39 (3) ◽  
pp. 505-513
Author(s):  
KU Ahammad ◽  
MM Rahman ◽  
MAM Molla ◽  
MG Azam
Keyword(s):  
Soil Moisture ◽  
Zea Mays L ◽  
Agricultural Research ◽  
Field Capacity ◽  
Research Field ◽  
Research Station ◽  
Maize Seeds ◽  
Moisture Regimes ◽  
Days To Maturity ◽  
Wet Condition

The experiment was conducted at the research field of Regional Agricultural Research Station, Jessore during two consecutive rabi seasons of 2008-2009 and 2009-2010 to find out the effect of hydropriming on the performance of maize seeds under variable soil moisture regimes. The treatments of the experiment were two priming methods viz., i) Hydropriming, ii) Non-priming and four moisture regimes viz., i) Wet condition, ii) Field capacity, iii) 75% of field capacity, and iv) 50% of field capacity. Results showed that yield and yield contributing characters (plant population/m2, number of cobs/m2, length of cob, diameter of cob, 100-grain weight) were influenced significantly by hydropriming. Yield and yield contributing characters were highest when hydroprimed seeds were sown at field capacity whereas it was the lowest at 75% of field capacity from non- primed seeds. Days to tasseling, days to silking, and days to maturity were reduced when hydroprimed seeds were sown at field capacity. At 50% of field capacity, no germination was occurred. DOI: http://dx.doi.org/10.3329/bjar.v39i3.21993 Bangladesh J. Agril. Res. 39(3): 505-513, September 2014

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