Influence of Potassium Substitution by Rubidium and Sodium on Growth,Ion Accumulation,and Ion Partitioning in Bean under High Alkalinity

ABSTRACT

The effects of partial and complete substitution of potassium (K⁺) by rubidium (Rb⁺) and sodium (Na⁺) on plant growth and ion accumulation and partitioning was studied in bean young plants cultivated in nutrient solution with or without bicarbonate (HCO₃ ^?)-induced alkalinity. Plant growth was significantly decreased due to alkalinity and the substitution of K⁺, being leaves more affected than roots. Rubidium caused a severe toxicity reflected in a reduction in root dry mass and total chlorophyll concentration. Ion partitioning was markedly altered by alkalinity. Content of nitrogen (N), calcium (Ca), magnesium (Mg), iron (Fe), K, and Na were more accumulated in the roots in HCO₃ ^?-treated plants, while decreased in the shoot. Iron (Fe) was accumulated at similar extent in plants with and without high alkalinity, except in plants grown in Rb⁺ solutions. However, Fe was more accumulated in the roots, suggesting that chlorophyll synthesis was impaired by reduced translocation or internal inactivation of Fe. Zinc total uptake was severely reduced under high alkalinity in plants grown in Na⁺ solutions, maybe due to decreased Zn activity. Calcium was translocated more actively to the leaves and Mg was accumulated more in the roots of plants in Na⁺solutions. Despite the severe decrease in plant dry mass caused by Rb⁺, there was a higher translocation of N, phosphorus (P), Ca, Mg, Fe, zinc (Zn), copper (Cu), and manganese (Mn) from the roots to the leaves.     

Arbuscular Mycorrhizal Fungi Enhance Tolerance of Rosa multiflora cv. Burr to Bicarbonate in Irrigation Water

ABSTRACT

High bicarbonate (HCO₃ ^?) of irrigation water can be detrimental to plant growth in sustainable horticultural production systems. The ability of arbuscular mycorrhizal fungi (AMF), ZAC-19, (composed of Glomus albidum, Glomus claroideum, and Glomus diaphanum) to enhance tolerance to HCO₃ ^? was tested on Rosa multiflora cv. Burr. Arbuscular mycorrhizal colonized and non-inoculated (non-AMF) plants were treated with 0, 2.5, 5, and 10 mM HCO₃ ^?. Increasing HCO₃ ^? concentration and associated high pH and electrical conductivity (EC)—reduced plant growth, nutrient uptake, and acid phosphatase activity, while increasing alkaline phosphatase activity (ALP). Inoculation with AMF enhanced plant tolerance to HCO₃ ^?, as indicated by greater growth (leaf, stem, and total plant dry weight, leaf area and leaf area ratio), leaf elemental concentration [nitrogen (N), phosphorus (P), potassium (K), calcium (Ca), iron (Fe), zinc (Zn), aluminum (Al), boron (B)], leaf chlorophyll concentration, higher mycorrhizal inoculation effect, lower root Fe reductase activity, and generally lower soluble ALP activity. While AMF colonization was reduced by increasing HCO₃ ^? concentration, colonization still occurred at high HCO₃ ^? concentration. At 2.5 mM HCO₃ ^?, AMF plant growth was comparable to plants at 0 mM HCO₃ ^?, further indicating the beneficial effect of AMF for alleviation of HCO₃ ^? plant stress.     

The influence of the growth media and mineral nutrition on corn root hydrogen / bicarbonate releases and rhizosphere pH

A study was made of the influence of substrate on the root releases of hydrogen ions (H+) and bicarbonate ions (HCO₃ ^‐) by corn (Zea mays, cv.Dea) grown between the 5/6 leaf and the 9/10 leaf stage in two different growth media, siliceous or calcareous sand. Different nutrient solutions were supplied in separate experiments, but in all cases, nitrogen was in the form of nitrate (NOg"), and iron chelates were present in solution.

In siliceous sand the pH generally increased, but acidification appeared with low NO₃ ^‐ nutrition. Roots released H⁺ and HCO₃ ^‐ simultaneously, and these ions partially reacted to form H₂CO₃. The pH variations depended on the balance of the released ions and on the low buffer capacity in this slightly acidic pH range. The algebraic sum of the ion effluxes was approximately equal to the sum of the ion uptakes; no stoichiometric coupling between the total H⁺ effluxes and the NO₃ ^‐ or potassium (K⁺) uptakes was recorded.

In calcareous sand HCO₃ ^‐ was released by the roots, but the H⁺ seedling effluxes always acidified the solutions with regard to the reference solutions in calcareous sand without plants. Even though HCO₃ ^‐ was released in great quantities by plants, the pH of the solutions did not become alkaline because of the high buffer capacity of the solution in contact with the calcareous medium. In this environment the plants reacted to the high levels of HCO₃ ^‐ and showed symptoms of lime‐induced chlorosis. To overcome the poor physicochemical conditions, H⁺ was released from the corn roots, and this H⁺ efflux was correlated to the total alkalinity of the solution.     

Arsenic Uptake from Arsenic-Contaminated Water Using Hyperaccumulator Pteris vittata L.: Effect of Chloride, Bicarbonate, and Arsenic Species

High As groundwater normally contained high concentrations of Cl^? and HCO ₃ ^? . This study examined the effects of Cl^?, HCO ₃ ^? , and As species on As uptake by hyperaccumulator Pteris vittata. Plants were exposed hydroponically to 5.0?mg/L As(III) or As(V) in the presence of 0, 0.5, 1, 2, 5, 10, and 20?mM of Cl^? or HCO ₃ ^? for 10?days. Addition of high Cl^? concentrations (>10?mM) slightly inhibited P. vittata growth (biomass), while generally had no significant effect on plant As uptake. High solution pH resulted in reduced plant growth and As uptake, which attributed to the inhibitory effects in HCO ₃ ^? treatments with the high pH of the high HCO ₃ ^? concentration. It was speculated that addition of HCO ₃ ^? (<20?mM) would have no significant effect on plant growth and As uptake. The inhibitory effect of HCO ₃ ^? on As translocation was less apparent in the As(III) solutions than the As(V) solutions. For the high As groundwater with As(III) as the predominant species, high pH, instead of high concentrations HCO ₃ ^? and Cl^?, was expected to inhibit As uptake. The results suggested that optimum plant growth and maximum As hyperaccumulation could be achieved by adjusting solution pH in the growth media (around 7.2).     

Effect of rate of nitrapyrin and source of N on soil pH and response of burley tobacco

Abstract

A field experiment was conducted on Maury silt loam soil (Typic Paleudalf) during 2 years to determine the effects of rate of nitrapyrin and source of N fertilizer on soil pH and response of burley tobacco (Nicotiana tabacum L.cv.^xKy‐14'). All sources of N were applied at the rate of 280 kg N ha^‐1. The information was needed to increase the efficiency of N fertilizer use and improve the growth and safety of tobacco.

Results indicated that application of a NO₃ ^‐source of N fertilizer or low rates of nitrapyrin (0.56 to 2.24 kg ha^‐1) decreased surface soil acidification and the concentration of plant Mn, while plant dry weight early in the growing season was increased. The early growth benefits noted for .nitrapyrin did not lead to increased cured leaf yields or value. Cured leaf yield and value were highest in plots receiving Ca(NO₃)₂, followed by KH₄NO₃, then urea.

Concentration of protein N, total alkaloids, and total volatile nitrogenous bases of cured leaves increased and NO₃ ^‐‐N decreased as rate of nitrapyrin increased. Total N concentration of cured leaf, however, was not significantly affected by nitrapyrin application, indicating that the proportion of absorbed N as NH₄ ⁺increased as nitrapyrin rate increased.     

Method for estimation of CO2(aq) plus H2CO3°, HCO3− and pH in soil solutions collected under field conditions

A method for the collection of soil solution and the determination of pH, H₂CO₃* (= CO₂(aq) plus H₂CO₃°), HCO₃^? and CO₃^2?, was developed which excluded atmospheric gases during the entire procedure. The soil solution was collected by tension lysimeters without exposure to the atmosphere. Using a closed system, the sample was transferred to a titration beaker for the analysis of pH, H₂CO₃* and HCO₃^?. The analysis of CO₂-acidity was done by titration with 0.0454 N Na₂CO₃ to the end point pH of 8.3. It was immediately followed by an acidimetric titration for the determination of alkalinity using 0.005 N H₂SO₄ under gentle N₂ flow; the equivalence point was determined graphically from the titration curve. In standard solutions, this method gave nearly 100% recovery of H₂CO₃* and HCO₃^?. In soil solutions, the pH markedly increased and H₂CO₃* decreased upon exposure to the atmosphere. The values of the sum of CO₂-acidity and alkalinity in soil solutions at a depth > 5 cm agreed well with the values of total inorganic carbon obtained by CO₂ infrared detection following CO₂ degassing. For solutions obtained from 100 cm and 300 cm depth (limestone) the measured distribution of H₂CO₃* and HCO₃^? was in agreement with the calculated values based on pH-measurement and total inorganic carbon. This comparison was unsatisfactory for the concentration of H₂CO₃* in solutions of the surface (0–15 cm) soil, possibly because the mathematical model as well as the interpretation of the titration curves did not consider any organic compounds in the solution.     

Use of CaCl2 to decrease ammonia volatilization after application of fresh and anaerobic chicken slurry to soil

Ammonia losses after surface application of fresh chicken slurry (15% solids) and anaer-obically stored chicken slurry (10% solids) to a silty clay soil (pH 6.9) at a rate equivalent to 34 m³ ha^?1 were studied in a laboratory incubation experiment. Total NH₃-N losses amounted to 29% of the initial uric acid-N+urea-N+NH⁺₄-N content of the fresh slurry and 28% of the initial NH⁺₄-N content of the anaerobic slurry. Peak rates of ammonia volatilization took place between 24 h and 48 h after application of the fresh slurry and within 5 h of application of the anaerobic slurry. The addition of CaCl₂ at a rate of 36 mg Ca g^?1 (dry wt) slurry decreased peak rates of ammonia volatilization from the fresh slurry by 73% and total losses by 37%. The decrease in total ammonia losses through CaCl₂ addition to the anaerobic slurry was only 8 %. The addition of CaCl₂ decreased CO₂ output from both slurries through precipitation of HCO₃^? as CaCO₃, thereby removing a source of alkalinity from the solution. The failure of the CaCl₂ addition to decrease significantly ammonia losses from the anaerobic slurry suggested that HCO₃^? was an important source of alkalinity driving ammonia volatilization in the fresh slurry, but not in the anaerobic slurry. CaCl₂, addition did not affect urea hydrolysis, nor net nitrogen mineralization. The decrease in ammonia loss achieved through CaCl₂ addition was however not associated with a parallel increase in ammonium concentrations in the soil. Further experiments showed that the ammonia retained by the CaCl₂, was probably fixed by the soil and rendered non-extractable by KCl.     

Effect of excess MgSO4 or Mg(HCO3)2 in irrigation water on corn growth

Abstract

Some irrigation waters have a high Mg/Ca ratio. The objective of the experiment reported herein was to compare the effect of high Mg in combination with different anions and different EC levels on the growth of corn (Zea mays L.). Corn was grown in the greenhouse in a calcareous soil equilibrated and irrigated with the following waters: 1) tap water (check, EC = 0.078 dS/m, SAR = 0.1); 2) Mg(HCO₃)₂, EC=1 dS/m; 3) Mg(HCO₃)₂, EC = 3; 4) MgSO₄₎ EC=1; 5) MgSO₄, EC=3; 6) MgSO₄, EC = 6; and 7) and 8) mixed salts (Ec = 3 & 6 dS/m, SAR = 5, Ca: Mg = 3: 1, Cl: SO₄ = 2: 1). Yield depressions of top growth caused by mixed‐salt waters (EC = 3 & 6) were 17 and 26%, respectively, compared to yields obtained with tap water. Single‐salt MgSO₄ waters (EC = 1, 3 & 6) reduced corn tops 19, 38, and 59%, respectively, more than the mixed‐salt solutions at equivalent soil salinity levels probably due to Mg‐induced Ca deficiency. The Mg(HCO₃)₂ waters (EC = 1 & 3) reduced top growth 45 and 87% more than the mixed salt solutions. Thus Mg (HCO₃)₂ was more than twice as depressive on corn top growth as MgSO₄. Corn root growth depression was similar to top growth depression. Leaf Ca: Mg ratio was related to their ratio in the soil solution. The leaf Ca and Mg concentrations were almost the same for plants irrigated with Mg(HCO₃)₂ or MgSO₄ at EC = 1. Therefore, Mg: Ca ratio of leaves did not explain the yield differences between the two Mg salts. Nutrient imbalances and a high pH of 9 were possibly responsible for the lower yields in the presence of Mg(HCO₃)₂.     

Response of Corn Growth in Salt‐Affected Soils of Northeast China to Flue‐Gas Desulfurization By‐product

Abstract

In semiarid and arid regions, plant growth is limited by high pH, salinity, and poor physical properties of salt‐affected soils. A field experiment was conducted in the semiarid region of Kangping in northeast China (42°70′ N, 123°50′ E) to evaluate a soil‐management system that utilized a by‐product of flue‐gas desulfurization (FGD). Soil was treated with 23,100 kg ha^?1 of the by‐product. Results of corn growth were grouped into three grades (GD) according to stages of corn growth: GD1, seeds did not germinate; GD2, seeds germinated but corn was not harvested; and GD3, plants grew well and corn was harvested. The pH, electrical conductivity (EC), bicarbonate (HCO₃ ^?), carbonate (CO₃ ^2?), exchangeable and soluble calcium (Ca²⁺), chloride (Cl), and sulfate (SO₄ ^2?) in surface soils of the three grades (>20 cm) was measured to assess the correlation between corn growth and soil properties. Vertical differences in subsoil properties (0‐100 cm) between GD1 and GD3 were compared to known benchmark soil profiles. The FGD by‐product significantly increased EC, exchangeable and soluble Ca²⁺, and SO₄ ^2? and decreased CO₃ ^2?, exchangeable sodium (Na⁺), and soluble Na⁺. pH, EC, HCO₃ ^?, CO₃ ^2?, and Cl^? were higher in surface soils of GD1 than GD3. Soil hardness, soil moisture content, Cl^?, and calcium carbonate (CaCO₃) were higher in GD1 than in GD3, whereas the amount of available P was lower in GD1. Interestingly, the concentration of Cl^?, a toxic element for plant growth, was 2.5 and 1.5 times higher in GD1 than in GD3 and control soil, respectively. In the comparison study of subsoils, GD1 and GD3 were classified as having typical characteristics of saline‐alkali soil (pH>8.5; exchangeable‐sodium‐percentage [ESP]>15; EC>4.0) and alkali soil (pH>8.5; ESP>15; EC<4.0), respectively.     

GROWTH AND NUTRITION OF YOUNG BEAN PLANTS UNDER HIGH ALKALINITY AS AFFECTED BY MIXTURES OF AMMONIUM,POTASSIUM, AND SODIUM

High concentrations of bicarbonate (HCO^? ₃) cause alkalinity of irrigation water and are associated with suppression in plant growth and micronutrient deficiencies, such as iron (Fe) and zinc (Zn). Because reports indicate that the deleterious effects of alkalinity may be counteracted partially by supplementary potassium (K⁺) or ammonium (NH₄ ⁺) an experiment was designed to evaluate the response of bean plants (Phaseolus vulgaris L.) grown in high alkalinity conditions to varying proportions of NH₄ ⁺, K⁺, or sodium (Na⁺) (as a potential substitute for K⁺). Plants established in a growth chamber were grown in hydroponics for 21 days in solutions containing 5 mM HCO^? ₃ and a total of 5 mM of a mixture of NH₄ ⁺, K⁺, and Na⁺. The proportions of NH₄ ⁺, K⁺, and Na⁺ were designed according to mixture experiment methodology. Total N in all the mixture treatments was maintained at 10 mM by using nitrate (NO^? ₃)-N, thus the NH₄ ⁺:NO^? ₃ ratio varied according to the proportion of NH₄ ⁺ in the mixtures. Alkalinity caused suppression in plant growth and chlorophyll concentration in the younger leaves, whereas excessive NH₄ ⁺ was associated with leaf scorching and decreased leaf expansion. High proportions of K⁺ alleviated alkalinity symptoms and produced higher shoot and root dry mass provided that NH₄ ⁺ was included in the mixture. However, a proportion of NH₄ ⁺ higher than 0.333 in the mixture (>1.66 mM NH₄ ⁺) induced toxicity. The highest shoot dry mass occurred if the NH₄ ⁺:NO^? ₃ ratio was 0.19:0.81 and the NH₄ ⁺:K⁺:Na⁺ proportion was 0.38:0.38:0.24 (1.9 mM NH₄ ⁺ + 1.9 mM K⁺ + 1.2 mM Na⁺). Thus, an improvement in plant growth is achieved when NH₄ ⁺, K⁺, and Na⁺ are blended together, in spite of the high alkalinity treatment imposed. Optimum NH₄ ⁺ was associated with a decrease in solution pH and an increase in shoot Fe and Zn concentration.     

Nutrient‐solution techniques for evaluation of iron efficiency of soybean 1

Abstract

The iron (Fe) efficiency of soybean [Glycine max (L.) Merr.] genotypes generally has been evaluated in the field on calcareous soil. A nutrient‐solution system has been developed to permit evaluation of Fe efficiency throughout the year. The objectives of this study were to assess the effectiveness of nutrient‐solution tests for evaluating the Fe efficiency of soybean genotypes and to evaluate alternative nutrient‐solution techniques that could minimize the cost of labor and chemicals. Five bicarbonate (HCO₃ ^‐) concentrations and three solution‐change schedules were evaluated in a factorial arrangement. Eight soybean genotypes with a wide range of Fe efficiency were evaluated in each treatment and in replicated field tests on calcereous soil during 3 years. Rank correlation coefficients between mean chlorosis scores of genotypes in nutrient solution and field tests ranged from 0.81 to 0.91 for the three solution‐change schedules and from 0.85 to 0.89 for the five HCO₃ ^‐ concentrations. Replacing the solution every 4 d was not superior to replacing it only at each stage of plant development or not changing the solution throughout the test. A stepwise increase in HCO₃ ^‐ level at each stage of plant development was not superior to utilizing a constant level of HCO₃ ^‐ throughout the test. The most economical evaluation of the Fe efficiency of soybean genotypes in nutrient solution can be achieved with no change in the solution and one or more HCO₃ ^‐ levels that are held constant throughout the test.     

Effects of aluminium ions on uptake of calcium,magnesium and nitrogen in Betula pendula seedlings growing at high and low nutrient supply rates

The effects of aluminium on plant nutrition in small birch plants (Betula pendula Roth) were investigated. By using relative addition rate (r _A, g g^?1 d^?1) of nutrients as the growth-controlling variable, it was possible to grow the plants at very low external nutrient concentrations and to simulate plant requirements at two different fertility levels. Before aluminium addition the plants were at steady-state relative growth rate, (R _G, g g^?1 d^?1). The two addition rates were free access of nutrients with R _G ≈ 0.215 d^?1, or nutrient-limited, R _Aand R _G=0.10 d^?1. Internal concentrations of calcium and magnesium decreased with increasing Al³⁺ conncentration in the nutrient solution while nitrogen concentrations in the plants remained unchanged or increased. It was demonstrated in both nutrition treatments that calcium and magnesium decrease per se does not reduce plant growth and that uptake has to be considered in relation to plant requirement at different growth rates. The interpretation of the effects of aluminium on Ca and Mg uptake and plant biomass development suggested that processes other than disturbances in Ca and Mg uptake are the cause of the decrease in growth.     

Occurrence of acidic groundwater in precambrian crystalline bedrock aquifers,Southwestern Sweden

The pH and alkalinity of groundwater from 7651 wells drilled in the Precambrian crystalline bedrock of southwestern Sweden has been evaluated. The wells are generally less than 100 m deep. Analytical results were collected from different laboratories and authorities in the region. In areas with thin soil cover or coarse-grained deposits overlying the bedrock, alkalinity is normally less than 100 mg HCO₃ L^?1. Below the marine limit, where clayey sediments predominate, alkalinity sometimes even exceeds 200 mg HCO₃ L^?1. When comparing pH and alkalinity of groundwaters from Quaternary deposits with bedrock groundwaters, the latter always have higher pH and alkalinity values. The most acidic bedrock groundwaters are found in small areas close to the city of Göteborg due to additional factors of high acid loadings, high groundwater discharge and thin soil layers. A study of data from 1949 to 1985 in the province of Värmland suggests that no regional acidification of importance is in progress. However, results from public water supplies support the hypothesis that the groundwaters which are most sensitive to acidification are those where discharge from wells in small bedrock aquifers induces rapid groundwater recharge of acidic surficial water.     

Iron chlorosis development and growth response of peach rootstocks to bicarbonate 1

For dicots, bicarbonate (HCO₃‐) is regarded as a main factor in the induction of iron (Fe) chlorosis in calcareous soils, and sand and solution culture. In sand culture experiments, peach [Prunus persica (Batsch) L.] rootstock developed chlorosis only when HCO₃‐ levels were equal to or higher than 6 mM. Above this level, chlorosis increaeed as HCO3‐ level was increased. In spite of the lack of chlorosis at to or below 6 mM of HCO₃‐, large growth reductions (40–60% reduction in fresh shoot weight) were seen in all rootstocks, although the tolerant rootstock had less reduction than the more susceptible rootstocks. Shoot growth was affected by HCO₃‐ more than was root growth.     

Rate of nitrapyrin and soil ph effects on nitrification of ammonium fertilizer and growth and composition of burley tobacco

Abstract

Laboratory and greenhouse experiments were conducted to determine the effects of rate of nitrapyrin and soil pH on nitrification of NH₄ ⁺ fertilizer in soil, and growth and chemical composition of burley tobacco (Nicotiana tabacum L. cv. ‘KY ‐14'). Such experiments were needed to develop information for increasing efficiency of N fertilizer use and to lessen the fertilizer‐induced soil acidity and salt effects on tobacco plants.

Results for laboratory and greenhouse incubations indicated that nitrification proceeeded slowly below pH 5.0 and the nitrapyrin necessary to delay nitrification increased with both increasing soil pH and length of incubation time. Generally, nitrification could be delayed 30 days by nitrapyrin rates of 0.25 or 0.5 μg g^‐1 regardless of soil pH. but rates of 1 μg g^‐1 nitrapyrin or higher were required for 60 days and longer incubation times, particularly at higher soil pH.

Growth and morphology of tobacco plants were either unaffected, or affected positively, by low rates of nitrapyrin (up to 2 μg g^‐1). However, rates of 4 μg g^‐1 and above reduced total plant dry weight, reducing sugars and contents of mineral elements. Concentrations and content of plant NO₃ ^‐ N and Mn were greatly decreased by application of nitrapyrin. Values for most parameters measured increased with increasing soil pH. The data show that low rates of nitrapyrin may be used to alter the ratio of NO₃ ^‐ to NH₄ ⁺ N absorbed by tobacco and possibly improve growth and safety of tobacco.     

Effect of bicarbonate on iron reduction by soybean roots 1

Release of reducing compounds by soybean (Glycine max (L.) Merr.] roots has been identified as an adaptive response mechanism to iron‐deficiency conditions which result in chlorosis. These compounds facilitate the conversion of Fe⁺³ to the metabolically active Fe⁺² form, allowing for increased uptake by roots in solution culture experiments. Degree of chlorosis is closely associated with HCO₃ concentration; however, the relationship between that ion and root reduction potential apparently has not been studied. We examined the effect of HCO₃‐ on root reduction potential of ten commercially‐grown soybean cultivars known to differ in chlorosis expression in the field. Root reduction potential was measured spectrophotometrically at 594 nm on samples of nutrient solution containing reduced Fe⁺² . Plants were grown with 5 mM NaHCO₃ or in HCO₃ ^‐‐free solutions. Averaged over cultivars, 0.205 umoles Fe⁺³ were reduced in the HCO₃ ^‐‐free solutions while only 0.009 umoles Fe⁺³ were reduced in the solutions containing HCO₃ ^‐. No significant differences were observed among cultivars for root reduction potential within either HCO₃ ^‐ treatment. Results from this study suggest that HCO₃ ^‐ may inhibit iron absorption by limiting the ability of roots to release reducing compounds which make available Fe⁺2 in the soil solution. This may partially explain the role of HCO₃ ^‐ in reducing chlorosis.     

Survey of molybdenum fertility status in Maryland coastal plain soils for tobacco production

Abstract

Coastal Plain soils in southern Maryland are typically acid (pH = 5.0±0.5) with low organic matter (1.2±0.5%), clay (2.8 to 9.8%), CEC (2.4 to 6.8 meq 100/g), and total Fe contents (4.5 to 34.9 g/kg). The objectives of this investigation were to assess the status of plant available molybdenum (Mo) in these soils by examining the extractable Mo levels in Ap horizon soil samples and tissue Mo contents in cured tobacco collected across a five‐county region. Seventy soil samples representing 11 soil series and 198 composite samples of tobacco served as the basis for the surveys. Plant available Mo in soil, estimated using a solution containing 0.18M ammonium oxalate and 0.1M oxalic acid as the extractant, ranged from 0.02 to 0.53 (ig/g and averaged 0.08 μg/g Mo. Three of the 11 soil series examined and 30% of the total soil samples exhibited extractable Mo levels ≤ 0.03 μg/g therefore may have less than adequate available Mo for tobacco. Cured leaf Mo contents ranged from non‐detectable to 7.95 μg/g and averaged 0.84±0.95 μg/g Mo. Approximately 15% of the leaf samples contained ≤ 0.2 μ/g Mo which approaches borderline deficiency for Mo with 12.2% having Mo contents within the range 0.2 to 0.4 ng/g where growth responses were reported in burley tobacco. The causes for the approximate one fourth of the plant samples having less than optimum Mo concentrations for maximum productivity for tobacco can likely be attributed to: 1) acid soils associated with inadequate liming programs; 2) very low extractable Mo levels in several soil series; and 3) excess input of SO₄ ^‐2 in fertilizers and acid rainfall in the region which have been shown to inhibit MoO₄ ^‐2 ion uptake by tobacco plants.     

Relations between lake acidification and sulfate deposition in Northern Minnesota,Wisconsin, and Michigan

From a level of 1 kg ha^?1yr^?1 in north central Minnesota, emission-related wet SO₄ deposition increases across northern Wisconsin and northern Michigan to about 18 kg ha^?1yr^?1 in south central Michigan. Samples taken from 82 clearwater (low color) lakes across this region in the summer of 1984 showed a pattern of acidification in proportion to deposition. We found a linear increase in the difference between alkalinity and Ca+Mg and in lake SO₄ concentration with increasing deposition. We developed a simple equation to predict the emission-related SO₄ deposition levels that will cause the alkalinity of sensitive clear-water lakes to go to zero.     

Response of Manzanillo olive transplants to different nitrogen and cobalt applications

A pot experiment was carried on ‘Manzanillo’ olives transplants included three levels of nitrogen (N) (N₁=25, N₂=50 and N₃=75 g N plant^?1 year^?1) and four levels of cobalt (Co) (B₁=zero, B₂=10, B₃=20 and B₄=30 ppm Co). Generally, fertilizing with 50 g N plant^?1 year^?1 gave the highest significant value than those of other treatments in all vegetative growth characters. Vegetative growth was gradually increased by increasing cobalt up to 20 ppm and 30 ppm levels. Regarding the combination between nitrogen and cobalt levels in most cases, the best treatment was N₂ x B₃, which gave the highest values of vegetative growth characters. The combinations of nitrogen and cobalt created slightly more variable and increased effects on the macro and micronutrient contents of ‘Manzanillo’ olives transplants.     

Underestimation of Available Phosphorus by Resin–Bicarbonate and Olsen Tests in Calcareous Soils treated with Gypsum

In the present study, Olsen [0.5 M sodium bicarbonate (NaHCO₃), pH 8.5] and resin–bicarbonate (HCO₃) tests underestimated available phosphorus (P) in calcareous soils treated with gypsum (CaSO₄). The reaction of CaSO₄ and HCO₃ ^? ion or resin–HCO₃ to form calcium carbonate (CaCO₃) precipitate reduced the strength of the Olsen NaHCO₃ extractant and resin–HCO₃ strip for P extraction. The iron (Fe) oxide–impregnated filter paper (Pi strip) was independent of CaSO₄ influence and thus correctly estimated soil‐available P with respect to plant response to soil‐available P. Two greenhouse experiments were conducted with maize and wheat grown on calcareous soils treated with different rates of CaSO₄. The results confirmed that Olsen and resin–HCO₃ tests should not be used to measure available P or labile P in the P fractionation scheme in the calcareous soils containing significant amounts of gypsum.