Supplemental soil sulphur increases cabbage yield

1996 ◽  
Vol 76 (4) ◽  
pp. 857-859 ◽  
Author(s):  
K. R. Sanderson ◽  
J. B. Sanderson ◽  
J. A. Ivany
Keyword(s):  
Key Words ◽  
Soil Ph ◽  
Prince Edward Island ◽  
Sandy Loam ◽  
Loamy Sand ◽  
Potassium Sulphate ◽  
Marketable Yield ◽  
Soil Application ◽  
Sulphate Sulphur ◽  
Effect On Yield

Marketable yield of cabbage (Brossica oleracea L. var. capitata) was significantly increased from 11 to 14% by a soil application of sulphur-containing materials, potassium sulphate and gypsum, on sandy loam to loamy sand soils in Prince Edward Island. Calcite had no effect on yield. Gypsum resulted in the highest yield on five sites. Potassium sulphate and gypsum increased leaf S concentration 0.70 and 1.45% respectively. Gypsum decreased while calcite increased soil pH. Key words: Cabbage, calcite, calcium, gypsum, potassium sulphate, sulphur

Effect of gypsum and elemental sulphur on calcium and sulphur content of rutabagas in Podzolic soils

2002 ◽  
Vol 82 (4) ◽  
pp. 785-788 ◽  
Author(s):  
K. R. Sanderson ◽  
M. R. Carter
Keyword(s):  
Key Words ◽  
Soil Ph ◽  
Prince Edward Island ◽  
Sandy Loam ◽  
Leaf Tissue ◽  
Field Studies ◽  
Elemental Sulphur ◽  
Yield Response ◽  
Marketable Yield ◽  
Podzolic Soils

Both studies and information are lacking concerning Ca and S nutrition of rutabagas (Brassica napobrassica Mill). Five field studies were conducted to determine yield response of rutabagas to soil-applied gypsum (CaSO4·2H2O), lime (calcite) and elemental S on sandy loam to loamy sand Orthic Podzols in Prince Edward Island. Marketable yield of rutabagas was not affected by addition of Ca or S amendments. Gypsum increased the S content of rutabaga leaf tissue and reduced soil pH. In this study, a soil extractable Ca level of at least 318 µg g-1 soil appears adequate to support rutabaga growth. Key words: Rutabagas, calcium, gypsum, calcite, elemental sulphur

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

Comparison of oxidoreductive enzyme activities in three coal tar creosote-contaminated soils

Soil Research ◽  
2019 ◽  
Vol 57 (8) ◽  
pp. 814 ◽  
Author(s):  
Arkadiusz Telesiński ◽  
Teresa Krzyśko-Łupicka ◽  
Krystyna Cybulska ◽  
Barbara Pawłowska ◽  
Robert Biczak ◽  
...  
Keyword(s):  
Contaminated Soils ◽  
Sandy Loam ◽  
Coal Tar ◽  
Loamy Sand ◽  
Clay Loam ◽  
Oxidoreductase Activity ◽  
Sandy Clay Loam ◽  
Sandy Clay ◽  
Polycyclic Aromatic ◽  
Negative Effect

This study used laboratory experiments to compare the effects of coal tar creosote on the activity of oxidoreductive enzymes in sandy loam, loamy sand and sandy clay loam soils. Different amounts of coal tar creosote were added to soil samples as follows: 0 (control), 2, 10 or 50 g kg–1 dry matter. The activity of soil dehydrogenases (DHAs), o-diphenol oxidase (o-DPO), catalase (CAT), nitrate reductase (NR) and peroxidases (POX) was determined. Contamination of soil with coal tar creosote affected oxidoreductase activity. Oxidoreductive enzyme activity following soil contamination with coal tar creosote was in the following order: DHAs > CAT > NR > POX > o-DPO in loamy sand and in sandy loam; and DHAs > POX > CAT > NR > o-DPO in sandy clay loam. The index of soil oxidoreductive activity (IOx) introduced in this study confirms the negative effect of coal tar creosote on oxidoreductase activity in soil. DHAs were the most sensitive to the contamination of soil with coal tar creosote. Moreover, the greatest changes in oxidoreductase activities were observed in loamy sand. Knowledge of the mechanism underlying the effects of coal tar creosote on oxidoreductive processes may enable development of a method for the bioremediation of polycyclic aromatic hydrocarbon-contaminated soils.

Soil acidity in 1970 and 1989 in a coniferous forest in southwest Finland

1998 ◽  
Vol 78 (3) ◽  
pp. 477-479 ◽  
Author(s):  
C. J. Westman ◽  
S. Jauhiainen
Keyword(s):  
Key Words ◽  
Soil Ph ◽  
Soil Acidity ◽  
Mineral Soil ◽  
Coniferous Forest ◽  
Soil Layers ◽  
Water Suspension ◽  
Ph Values ◽  
Humus Layer ◽  
Repeated Sampling

Forest soil pH in southwest Finland was measured with identical sampling and analysing methods in 1970 and 1989. The acidity of the organic humus layer increased significantly as pH values measured on water and on salt suspensions decreased between the two sampling dates. For the mineral soil layers, no unambiguous trend was found. pH values measured on salt suspension tended to be unchanged or lower, while pH on water suspension in some soil layers were even higher in 1989 than in 1970. Key words: pH, repeated sampling

THE EFFECT OF ANTECEDENT FREEZE-THAW FREQUENCY ON RUNOFF AND SOIL LOSS FROM FROZEN SOIL WITH AND WITHOUT SUBSOIL COMPACTION AND GROUND COVER

1989 ◽  
Vol 69 (4) ◽  
pp. 799-811 ◽  
Author(s):  
LINNELL M. EDWARDS ◽  
J. R. BURNEY
Keyword(s):  
Prince Edward Island ◽  
Sandy Loam ◽  
Bare Soil ◽  
Winter Rye ◽  
Rainfall Simulator ◽  
Fine Sandy Loam ◽  
Freeze Thaw ◽  
Sediment Loss ◽  
Freezing Period ◽  
Subsoil Compaction

Three soils from Prince Edward Island (a loam, a fine sandy loam, and a sandy loam) were tested under a laboratory rainfall simulator to examine the effects of frequency of freezing and thawing, winter rye cover, incorporated cereal residue, and subsoil compaction on runoff volume and sediment loss. Wooden soil boxes were subjected to simulated rain (i) at the end of a 10-d freezing period, and (ii) at the end of the 5th 24-h freezing period of a 10-d alternating freeze-thaw cycle (freeze/thaw). Where the soil was continuously frozen for 10 d, there was 178% greater sediment loss and 160% greater runoff than with daily freeze/thaw over the same period, but there was no difference in sediment concentration. Incorporated cereal residue decreased sediment loss to 50% and runoff to 77% of that from bare soil. Winter rye cover decreased sediment loss to 73% of that from bare soil. Simulated soil compaction caused a 45% increase in sediment loss. The loam soil showed 16.5% greater loss of fine sediment fractions <0.075 mm than the fine sandy loam which showed 23.4% greater loss than the sandy loam. Key words: Freeze-thaw, erosion, compaction, winter rye, cereal residue, rainfall simulator, Prince Edward Island soils

scholarly journals Effect of Potassium Humate and Micronic Sulfur on the Chemical Properties of Some Soils of Toshka, Egypt

2020 ◽  
pp. 1-9
Author(s):  
Atef A. A. Sweed ◽  
Ahmed A. M. Awad
Keyword(s):  
Soil Ph ◽  
Block Design ◽  
Chemical Properties ◽  
Agricultural Practices ◽  
Loamy Sand ◽  
Available P ◽  
Control Treatment ◽  
Soil Drainage ◽  
Potassium Humate ◽  
And Control

Low soil organic matter, low nutrient availability and the higher soil pH (more than 8) are the major problem of agricultural practices in region of Toshka. An incubation trial at October 2019 was conducted to investigate the effect of potassium humate (KH) and micronic sulfur (MS) on some chemical properties of different soils (sandy clay soils, loamy sand and sandy soils). The used amendments (KH and MS) were added to the studied soil at 4 levels of each amendment i.e. 0.0, 0.25, 0.50 and 1.0%. A two way randomized completely block design and provided with three replications. Studied parameters were included soil pH, EC, exchange Na and the content of available - P and K. Results showed that, the MS application at 1% level caused a significant decrease in soil pH values compared with the KH application and control treatment. These reductions were more pronounced in case of soil B (loamy sand). Also, KH application gave an increase on exchange Na and available-K. While MS application was cause an increased in soil EC and available-P in the three soils under study. Moreover, the increases in the percentage of available – K with added of KH were higher than added of MS for soils under study. While the percentages of available-P with added of KH were higher than with added of MS for studied soils. It may be recommended to add KH and MS at a rate of 1% to improve the soil chemical properties. But the effect of application from MS has greater than KH to increase dissolved sodium salts on the form of sodium sulfate, which facilitates disposal during soil drainage.

MINERAL ELEMENTS IN CEREAL GRAINS AND LEGUMES GROWN IN PRINCE EDWARD ISLAND

1987 ◽  
Vol 67 (2) ◽  
pp. 569-572 ◽  
Author(s):  
K. A. WINTER ◽  
U. C. GUPTA
Keyword(s):  
Trace Elements ◽  
Key Words ◽  
Prince Edward Island ◽  
Mineral Elements ◽  
Cereal Grains ◽  
Cattle And Sheep

Samples of barley, wheat, clover and alfalfa grown in Prince Edward Island were analyzed for Ca, P, K, Mg, Mo, S, Mn, Zn and Fe. Compared with the requirements for livestock, the cereal grains and forages tended to be low or deficient in several minerals. The need for a suitable trace-mineralized salt in cattle and sheep diets is indicated. Key words: Minerals, trace elements, grains, legumes

THE EFFECT OF CHLORINE ON THE HYGROSCOPICITY OF FLUE-CURED TOBACCO

1961 ◽  
Vol 41 (1) ◽  
pp. 195-198 ◽  
Author(s):  
J. M. Elliot ◽  
L. S. Vickery
Keyword(s):  
Loamy Sand ◽  
Chlorine Content ◽  
Moisture Uptake ◽  
Total Sugars ◽  
Effect On Yield ◽  
Effect Of Chlorine

Chlorine from 20 to 50 pounds per acre had no effect on yield or leaf-grade quality of flue-cured tobacco grown on a Fox loamy sand. Increased applications of chlorine increased the chlorine content, moisture uptake, and decreased the rate of burn of the cured leaf but had no effect on the amount of total sugars.

Prediction of available potassium in Ontario soils by electro-ultrafiltration and chemical extraction

1992 ◽  
Vol 72 (2) ◽  
pp. 159-167 ◽  
Author(s):  
Liangxue Liu ◽  
T. E. Bates ◽  
T. S. Tran
Keyword(s):  
Organic Matter ◽  
Soil Properties ◽  
Key Words ◽  
Soil Ph ◽  
Chemical Extraction ◽  
K Uptake ◽  
Chemical Methods ◽  
Exchangeable Calcium ◽  
Time Required

The extractions of soil K by electroultrafiltration (EUF) and by chemical methods were compared as predictors of plant-available K for greenhouse-grown alfalfa on 38 Ontario soils. The relation of soil properties to the amount of K extracted by EUF fractions was also examined. The contents of silt and clay were negatively correlated with EUF-K at 50 V and 22 °C and positively correlated with EUF-K at 400 V and 80 °C. Soil pH and organic matter were not significantly correlated with the amounts of K extracted in the EUF-K fractions. The EUF extraction of K was influenced by the presence of carbonate or high exchangeable calcium in soils. Similar correlations were obtained between K uptake and K extracted by chemical methods and the sum of EUF-K fractions. When used along with other soil properties, EUF-K fractions and K extracted by chemical methods predicted availability of soil K with roughly equal ability. The model using the sum of K extracted by EUF at 50, 200 and 400 V is the simplest one and contains three variables, K, K2 and Ca2. The use of EUF is limited due to cost of equipment and time required for analysis, unless a number of nutrients can be accurately determined on one extract. Among the chemical methods, equations developed using three nonacidic extradants, NaCl, ABDTPA and NH4OAc explained more variation in K uptake than two acidic extractants, Mehlich 3 and 0.1 M HNO3. The NaCl model, ABDTPA model and NH4OAc model contained the same variables and had similar R2 values (0.88–0.91). Key words: Available K, chemical methods, electro-ultrafiltration, EUF-K fractions, K uptake

scholarly journals IMPACT OF AGRO-ENVIRONMENTAL SYSTEMS ON SOIL EROSION PROCESSES AND SOIL PROPERTIES ON HILLY LANDSCAPE IN WESTERN LITHUANIA

2015 ◽  
Vol 24 (1) ◽  
pp. 60-69 ◽  
Author(s):  
Gintaras JARAŠIŪNAS ◽  
Irena KINDERIENĖ
Keyword(s):  
Soil Erosion ◽  
Soil Properties ◽  
Soil Ph ◽  
Soil Texture ◽  
Sandy Loam ◽  
Chemical Properties ◽  
Available Phosphorus ◽  
Erosion Processes ◽  
Physico Chemical ◽  
The Impact

The objective of this study was to evaluate the impact of different land use systems on soil erosion rates, surface evolution processes and physico-chemical properties on a moraine hilly topography in Lithuania. The soil of the experimental site is Bathihypogleyi – Eutric Albeluvisols (abe–gld–w) whose texture is a sandy loam. After a 27-year use of different land conservation systems, three critical slope segments (slightly eroded, active erosion and accumulation) were formed. Soil physical properties of the soil texture and particle sizes distribution were examined. Chemical properties analysed for were soil ph, available phosphorus (P) and potassium (K), soil organic carbon (SOC) and total nitrogen (N). We estimated the variation in thickness of the soil Ap horizon and soil physico-chemical properties prone to a sustained erosion process. During the study period (2010–2012) water erosion occurred under the grain– grass and grass–grain crop rotations, at rates of 1.38 and 0.11 m3 ha–1 yr–1, respectively. Soil exhumed due to erosion from elevated positions accumulated in the slope bottom. As a result, topographic transfiguration of hills and changes in soil properties occurred. However, the accumulation segments of slopes had significantly higher silt/clay ratios and SOC content. In the active erosion segments a lighter soil texture and lower soil ph were recorded. Only long-term grassland completely stopped soil erosion effects; therefore geomorphologic change and degradation of hills was estimated there as minimal.

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