Kriging analysis of soil properties

Background, aim, and scope

Soil as a landscape body contains wide ranges of physical, chemical, morphological, and mineralogical properties, both laterally and vertically. Soils with similar properties and environments are expected to behave similarly. A statement on land use potential will depend in part on the precision and accuracy of the statements that can be made about the soils. This information has some practical applications in optimizing land management and productivity improvement. The spatial patterns and dependence of some selected physicochemical properties of brackish marsh and surrounding soils were investigated using a 2-D kriging analysis in conjunction with a geostatistical (GS+, Michigan) model.

Materials and methods

Composite (four subsamples) surface samples (0–20 cm) were obtained across the sampling sites (717 ha). Sampling area was subdivided into north–south transect (NST) and east–west transect (EWT). Subsamples were mixed resulting in 40 composite samples. These samples were stored at 5°C until the different physical (particle size) and chemical analyses were initiated. Soil chemical analyses included electrical conductivity (EC), Cl^?1, pH, and water soluble Na, S, Ca, Mg, Fe, and Al by inductively coupled plasma spectroscopy (ICP). Soil extraction was performed via an automatic soil extractor. A 1:2 soil to extracting solution ratio was used for all the extractions. The concentration of Cl^?1 in the soil sample was determined using a chloride electrode (Model 94-17B). Some selected physicochemical properties were interpolated by kriging. The procedures of univariate/multivariate analyses and kriging techniques were followed to evaluate the spatial dependence of some selected physicochemical properties of soils in the landscape. The kriging procedures included preliminary data analysis, structural data analysis, log kriging estimations, and image generations of spatial results. Based on the results of the kriging study, a field study evaluating the effects of gypsum and water management on the yield response of selected species of marsh vegetation was conducted in the area where soil samples were taken for the kriging study. The overall yield responses of four species of marsh vegetation to gypsum addition (0 vs. 7 Mg ha^?1) and water management (flooded vs. non-flooded) were evaluated for joint grass (Paspalum vaginatum, SW.), marsh hay cordgrass (Spartina patens MuhL.), saltgrass (Distichlis spicata L.), and American three-square (Scirpus americanus Pers.).

Results

There was a significant spatial dependence and differences (p ≤ 0.01) for all soil parameters tested. The variability of an individual soil property, as indicated by coefficients of variation (CV), differed widely. Some soil properties in the lower horizons were more uniform than those at the surface because of fewer disturbances and effects of micro-topography. Soils may develop markedly contrasting morphologies and properties that may vary laterally (east–west) and vertically (north–south). There was no plant survival in the non-flooded plots except for the marsh hay cordgrass, which had an average survival rate of 32.8%. Plots receiving 7 Mg ha^?1 gypsum had significantly higher dry matter production than the control. Gypsum application increased dry matter yield (Mg ha^?1) of joint grass (4.6 to 9.2), marsh hay cordgrass (2.0 to 9.2), salt grass (0.9 to 3.2), and American three-square (1.5 to 3.0) in flooded soils.

Discussion

The successions of high and low micro-relief within landscapes that were identified via kriging analysis may affect the overall growth and biomass production of marsh vegetation. Many of the differences and spatial dependence of soil properties in the study area that vary with topography are because of some combinations of microclimate, soil pedogenesis, geological surficial processes, and the sorting effects of water movement. Plants in the flooded plots had much higher dry matter yield (DMY) than the plants in non-flooded plots. Both gypsum addition and water management should become a major part of any marsh revegetation program.

Conclusions

Kriging analysis of the landscape suggested that the majority of the spatial variability of some soil properties within the study area were caused by the interactive effect of micro-topography and hydrologic pattern. Spatial variability will therefore affect soil performance. A uniform application of any soil amendments like fertilizer or gypsum in the area that possessed spatially variable soil would result in an overapplication in some parts of the area and an underapplication in other areas. Plants that were grown in flooded plots with gypsum treatment of 7 Mg ha^?1 had a higher dry matter yield.

Recommendations and perspectives

Knowledge of the existing soil variability in the area can be utilized to develop a stochastic model that may describe the potential land use capabilities. The prediction is being made by matching the requirements of specific land use to the characteristics of soils in the landscape. Results of an investigation of this type are of great interest to environmental scientists, water resource planners, regulators, decision makers, engineers, soil scientists, and resource managers. Kriging results were suggesting that both gypsum addition and water management should become a major part of marsh revegetation and restoration programs.     

Carbon and nitrogen in a Ferralsol under zero‐tillage rotations based on cover,cash or hay crops

To identify crop rotation systems capable of sequestering C and N to 1 metre depth in a subtropical Ferralsol of Southern Brazil managed under long‐term zero‐tillage (21 yrs), we evaluated six crop sequences: wheat (Triticum aestivum)–soybean (Glycine max) [W‐S], the baseline; oat (Avena strigosa, as cover crop)–maize (Zea mays)–wheat–soybean [O‐M‐W‐S]; vetch (Vicia villosa, as legume cover crop)–maize–wheat–soybean [V‐M‐W‐S]; vetch–maize–oat–soybean–wheat–soybean [V‐M‐O‐S‐W‐S]; ryegrass (Lolium multiflorum, for hay)–maize–ryegrass–soybean [R‐M‐R‐S]; and alfalfa (Medicago sativa, for hay)–maize [A‐M]. Compared to W‐S and to 1 metre, the hay‐based system of A‐M showed the largest C and N sequestration rates (0.50 and 0.06 Mg/ha/yr, respectively). Alfalfa, being a perennial legume under cut‐regrowth cycles, possibly added more C and N through roots. The other hay system, R‐M‐R‐S, also sequestered C efficiently (0.27 Mg/ha/yr), but not N (0.01 Mg/ha/yr). The legume‐based system of V‐M‐W‐S sequestered significant amounts of both C (0.29 Mg/ha/yr) and N (0.04 Mg/ha/yr). The grass‐based system of O‐M‐W‐S showed the lowest sequestration of C (0.09 Mg/ha/yr). In all systems, a positive relationship (R² = 0.71) occurred between estimated addition of root C and soil C stock to 1 metre. Whenever C and N sequestration occurred, more than half of that occurred below 20 cm depth. Results suggest that adoption of legume‐based systems, perennially as A‐M or annually as V‐M‐W‐S, is efficient for C and N sequestration in subtropical zero‐tillage soils and that roots possibly contribute more to that sequestration than aboveground biomass.     

Effect of gypsum on soil potassium and magnesium status and growth of alfalfa

Abstract

Though surface‐applied gypsum has been shown to be useful in reducing the subsoil acidity syndrome, excessive application could reduce the availability of other essential cations in soil. This study was conducted to determine the effects of surface‐applied gypsum on the availability of potassium (K) and magnesium (Mg) in field soils. Field experiments were conducted on Davidson and Tifton series soils in the southeastern United States with 6 main ameliorant treatments (0, 2, 5, and 10 t gypsum/ha, soil profile mixed to 1 m without lime incorporation and, mixed with lime to 1‐m depth), and 2 levels of Mg (0 and 100 kg Mg/ha) and 4 levels of K (0, 125, 250, and 375 kg K/ha) in a split‐split plot configuration. Alfalfa was grown on the Tifton soil and sorghum on the Davidson soil. Yields of alfalfa and sorghum increased with 2 t gypsum/ha but were adversely affected above 5 t gypsum/ha. Gypsum amendment at 2 t/ha reduced topsoil exchangeable Mg and K in both soils. In the soil profile study, exchangeable Mg was reduced throughout the upper 52.5‐cm depth, while no reduction of K was observed below the 22.5‐cm depth in either soil. The study indicates that Mg is more susceptible to leaching loss than K after surface application of gypsum. It is also suggested that surface‐applied gypsum be used as a soil ameliorant along with proper management of Mg and K fertilizers.     

P ‐ Mo interactions on the yield and nodulation of white clover grown on limed‐lignite overburden materials

Abstract

A greenhouse study using lignite overburden surface soil from a lignite mine in northwest Louisiana was conducted to determine the yield response and nodulation of inoculated and non‐inoculated white clover (Trifolium repens L.) to P (0, 40, and 80 kg/ha) and Mo (0, 90, and 180 g/ha) fertilization. Results manifested a highly significant response of inoculated white clover to a single application of P and Mo. Application of P at the rate of 40 and 80 kg/ha increased the dry matter yield (DMY) of white clover by 164% and 154%, while Mo fertilization at the rate of 90 and 180 g/ha increased the dry matter yield (DMY) by 21% and 37%, respectively, over the control. The yield of white clover was also significantly affected by Rhizobium inoculation. Yield was increased from 2.1 to 2.5 Mg/ha which is equivalent to a 19% yield improvement over the non‐inoculated plants.

Nodule formation (NF), likewise, was significantly favored by P and Mo fertilization. Results also revealed that Rhizobium inoculation had remarkably improved the nodule count of white clover. Nodule count was increased from 0.4 to 5.5 or 1375% improvement between the inoculated and non‐inoculated plants. The non‐inoculated white clover also responded significantly to P fertilization, but not to Mo addition. Nodule formation, however, was not observed from the non‐inoculated white clover except at the highest rate of P and Mo additions. Increasing P supply significantly increased the concentrations of P, S, Na, and Ca but decreased the concentration of K in the clover. Mo additions resulted in increased concentrations of P and Ca. No significant P‐Mo interaction effects were observed on the nutrient concentration of white clover.     

Yield,quality and k/(Ca+Mg) ratio of tall fescue beeeding lines on amended and nonamended minesoil

Abstract

Surface mineable coal is abundant beneath many farmland areas in Missouri. Presently, 90% of the electricity generated in the state is by coal powered plants. Surface strip‐mining laws now require reclamation of these lands after drastic disturbance. Tall fescue (Festuca arundinancea Schreb) cultivars and breeding lines have been evaluated for yield, nutrient composition and quality on undisturbed lands, but not for these qualities and for adaptability to revegetate drastically disturbed lands.

Six breeding lines and 2 cultivars of tall fescue were evaluated for yield, nutrient composition, crude protein and IVDMD on limed and unlimed minesoils in west‐central Missouri. The experimental dersign was a randomized split‐block with lime treatment the split‐block, 3‐replications, with individual plots 1.21 x 3.05 m. Agriculture lime with ENM index of 291 at rate of 19 mt/ha was incorporated, fescue seeded and the experimental area mulched during August‐September, 1978. The 1979 harvest samples were composited for crude protein, nutrient and IVDMD analyses and the 1980 harvest samples were analyzed for individual plots.

The 1979 yield was not significantly different between genetic materials, but mean yield from limed minesoil was significantly higher than from unlimed minesoil. Yield data evaluation suggest Kenhy, WG3B, HMR to yield highest on unlimed minesoil and WG2B, LMR and HMR highest on limed minesoil, with MO‐96 lowest in yield limed or unlimed. The calculated K/(Ca+Mg) ratio of HMR and Kenhy was interpreted to be borderline for potential occurrence of grass tetany under limed environment. Differential divalent cation accumulation capacities of the breeding lines LMR and HMR was expressed on both the limed and unlimed minesoil. Potassium was not judged to reach a sufficiently high or Mg sufficiently low level to suggest potential problem of hypomagnesaema.

Lime increased IVDMD, but not crude protein. Crude protein varied by year, but IVDMD remained nearly constant. The genetic materials MO‐96 and H‐I accumulated higher quantities of Mg upon liming, but had lower IVDMD. Differences in yield were not significantly related to cation accumulation or forage quality on this minesoil, limed or unlimed.     

Yield,quality and K/(Ca+Mg) ratio of tall fescue breeding lines on amended and nonamended minesoil

Abstract

Surface mineable coal is abundant beneath many farmland areas in Missouri. Presently, 90% of the electricity generated in the state is by coal powered plants. Surface strip‐mining laws now require reclamation of these lands after drastic disturbance. Tall fescue (Festuca arundinancea Schreb) cultivars and breeding lines have been evaluated for yield, nutrient composition and quality on undisturbed lands, but not for these qualities and for adaptability to revegetate drastically disturbed lands.

Six breeding lines and 2 cultivars of tall fescue were evaluated for yield, nutrient composition, crude protein and IVDMD on limed and unlisted minesoils in west‐central Missouri. The experimental design was a randomized split‐block with lime treatment the split‐block, 3‐replications, with individual plots 1.21 × 3.05 m. Agriculture lime with ENM index of 291 at rate of 19 mt/ha was incorporated, fescue seeded and the experimental area mulched during August‐September, 1978. The 1979 harvest samples were composited for crude protein, nutrient and IVDMD analyses and the 1980 harvest samples were analyzed for individual plots.

The 1979 yield was not significantly different between genetic materials, but mean yield from limed minesoil was significantly higher than from unlimed minesoil. Yield data evaluation suggest Kenny, WG3B, HMR to yield highest on unlimed minesoil and WG2B, LMR and HMR highest on limed minesoil, with MO‐96 lowest in yield limed or unlimed. The calculated K/(Ca+Mg) ratio of HMR and Kenhy was interpreted to be borderline for potential occurrence of grass tetany under limed environment. Differential divalent cation accumulation capacities of the breeding lines LMR and HMR was expressed on both the limed and unlimed minesoil. Potassium was not judged to reach a sufficiently high or Mg sufficiently low level to suggest potential problem of hypomagnesaema.

Lime increased IVDMD, but not crude protein. Crude protein varied by year, but IVDMD remained nearly constant. The genetic materials MO‐96 and H‐I accumulated higher quantities of Mg upon liming, but had lower IVDMD. Differences in yield were not significantly related to cation accumulation or forage quality on this minesoil, limed or unlimed.     

Sulfate uptake by salinity‐tolerant plant species

Abstract

High soluble‐sulfate (SO₄) concentrations affect water quality, soil chemistry, plant sulfur (S) levels, and possibly ruminant‐animal health. The objective of this greenhouse pot study was to determine the potential for accumulating high levels of S by tansy mustard (Descurainia pinnata (Walt.) Britton), kochia (Kochia scoparia L. Schrad.), yellow sweet clover (Melilotus officinalis L.), slender wheatgrass (Elymus trachycaulus (Link) Gould ex Shinners), and sunflower (Helianthus annuus L.). Plants were grown on both a Brinegar (fine‐loamy Ultic Argixeroll) and Portneuf (coarse silty Durixerollic Calciorthid) soil. Each species received five‐SO₄ levels. The saturation extract electrical conductivity (EC) of the cropped soils ranged from 6 to 16 dS/m, while the soluble SO₄ varied from 16 to 200 mmol_c/kg soil. Soil solutions were saturated or very nearly saturated with respect to gypsum at the conclusion of each study. Plant dry matter yield, except of grass growing on the non‐calcareous soil, was not reduced by SO₄ treatment nor by the sulfate‐induced decrease in mole fraction of calcium (Ca)/(sum cations) to values less than 0.10 for kochia and grass. Sulfur concentration in the plants ranged from 2.5 mg/g in grass to 10 mg/g in mustard and for each species was linearly related to the SO₄ treatment and soil‐SO₄ activity. Plant SO₄‐S values ranged from 70 μg/g in the grass to nearly 900 μg/g in mustard. Total nitrogen (N): organic S was 4.4, 7.5, 11.4, 16.5, and 5.8 for mustard, kochia, clover, grass, and sunflower, respectively. It was concluded that these species could accumulate high levels of S in the above ground tissue.     

Yield response of soybeans to P and K fertilization as correlated with soil extractable and tissue nutritional levels

Abstract

Bragg soybeans [Glycine max. (L. ) Merill] were grown under field conditions near Sanford, Florida on a tile‐drained Immokalee fine sand (sandy, siliceous, hyperthermic Arenic Haplaquod). The objectives were: 1) to assess the K and P fertilizer requirements of soybeans grown in central Florida 2) to correlate soil and tissue nutritional levels with extractable soil nutrients and 3) to assess the influence of K application time on yield.

Experimental treatments were four K rates (0, 50, 100, and 200 kg K/ha), three P rates (0, 25, and 50 kg P/ha), and two sidedress K rates (0 and 50 kg K/ha) at early bloom. Treatments were arranged in a randomized complete block design and replicated four times.

Yield increased with each increase in applied K. Statistical maximum yield was obtained on plots which contained 103 ppm double‐acid extractable K during the pod‐filling stage of growth. Tissue K at early bloom exceeded 2.85% at maximum statistical yield. Potassium applied broadcast at early bloom did not significantly influence yield.

This soil contained approximately 390 ppm double‐acid extractable P prior to P application. No significant yield response to applied P was observed, indicating that the original extractable P content of the soil was adequate for the yield level obtained.

The quadratic regression of the ratio equivalents of double‐acid extractable K:Ca + Mg on the same ratio for the plant tissue is highly significant. This expression was a good predictor of tissue accumulation of these nutrients in that the coefficient for determination was 0.68.     

Foliar nutrient status in three boreal species for three years following hexazinone application

Abstract

Effects of hexazinone on the dynamics of macronutrients were studied in the foliage of trembling aspen, showy aster and marsh reed grass for three years after broadcast application of 10% granular formulation of hexazinone at 0, 2, and 4 kg ai/ha rates in August 1986 in a 3‐year‐old mixedwood cutover in a boreal forest. In untreated plots, nutrient concentrations followed normal patterns: calcium (Ca) increased from spring to late summer; potassium (K), phosphorus (P), sulfur (S), and nitrogen (N) peaked in early summer and declined towards fall; and magnesium (Mg) did not show any definite trends. At each sampling date, the coefficient of variation ranged from <10% for Ca, Mg, K and total N to 10–20% for P and S. Seasonal variations in the concentrations of each element were greater than the year‐to‐year variations. In treated plots, hexazinone application resulted in elevated concentrations of total Ca, Mg, K, P, S, and N during the first growing season, but these changes were only significant (P<0.05) at the 4 kg rate. The intensity of the effects declined by the end of the second growing season following herbicide application. In 1989, differences between nutrient levels in foliage from control and treated sites were significant (P<0.05) only for total N. Consequently, any changes in the nutrient status of hexazinone‐treated sites (beyond two years post‐treatment) are not expected to result from changes in foliar nutrient levels, but rather from changes in litter fall quantities, species dominance and total vegetation cover. Nutrient quality of forage for wildlife would not be affected beyond two years post‐treatment.     

Gypsum material effects on peanut and soil calcium

Abstract

Adequate availability of calcium (Ca) in the upper 7–10 cm of soil is extremely important for pod development and therefore for production of quality peanut (Arachis hypogaea L.). Supplemental Ca is usually applied as gypsum, however, availability of Ca may depend on the type of gypsum. The objective of a laboratory study was to evaluate recovery of Ca in Mehlich I, 0.01 M NaNO₃ and deionized water extractants from seven gypsum materials which varied physically from fine and coarse powders to crystals, granules and pellets. Overall, recovery of Ca was much greater in Mehlich I (89.5–99.6% of total Ca) than in either 0.01 M NaNO₃ (81.0–98.4%) or deionized water (78.7–97.5%). However, for 3 sources, recovery of Ca was very similar in NaNO₃ solution and deionized water.

Field experiments were conducted on Lakeland sand (Mehlich I Ca = 127 kg/ha, 0–15 cm) and Tifton loamy sand (Mehlich I Ca = 665 kg/ha) soils to study the effects of the gypsum materials on Florunner peanut grade and yield. Effects of gypsum treatments on Mehlich I‐ and 0.01 M NaNO₃‐extractable soil Ca were also evaluated during peanut pod development. On the Lakeland soil, Mehlich I Ca increased from 127 to a range of 420–737 kg/ha following application of gypsum depending on the type of gypsum material. Percent sound mature kernels were significantly greater where gypsum was applied than in the control treatment, regardless of source. Total sound mature kernel yield and gross return were greatest for the more soluble sources. The yield vs. soil test Ca relationship 90 d after planting revealed that yield response was very minimal if soil Ca was greater than 290 and 85 kg/ha of Mehlich I and 0,01 M NaNO₃‐extractable Ca, respectively. Application of gypsum to the Tifton soil, regardless of type of material, had no significant effect on yield, grade or gross return because Mehlich I extractable Ca in the control treatment was well over 560 kg/ha; the critical soil test Ca for runner peanut according to the current Georgia soil test recommendation.     

Effects of grass vegetation strips on soil conservation and crop yield under rainfed conditions in the Indian sub‐Himalayas

Vegetation strips (VS) along with conservation tillage, application of organic amendments and weed mulching improve crop yields by reducing run‐off and topsoil erosion. To investigate these issues, an experiment was conducted under rainfed conditions using grass VS for four and a half years (June 2007 to October 2011) at Dehradun, Uttarakhand, in the Indian Himalayan region. VS were incorporated in the experimental plots (Entisols) in a randomized complete block design in permanent 100 × 20 m (2000 m²) plots with a 2% slope to evaluate the effects of vegetation strips on run‐off, soil loss and crop yield. Three treatments were evaluated: (i) without VS with recommended NPK under conventional tillage, (ii) panicum as VS with recommended NPK under conventional tillage and (iii) palmarosa+ that consists of palmarosa as VS along with organic amendments (farmyard manure, vermicompost and poultry manure) and weed mulch under minimum tillage. The results show that soil loss and run‐off were significantly lower (P < 0.05) in plots under palmarosa+ than without VS treatment. Mean soil loss of 3.4, 5.2 and 7.1 t/ha was recorded from palmarosa+, panicum and without VS treated plots, respectively. Mean run‐off was 234, 356 and 428 mm from plots under palmarosa+, panicum and without VS, respectively. Maize yield was lower on the plots under palmarosa+ compared with panicum, but significantly higher (P < 0.05) than without a strip. The succeeding rainfed wheat yield was significantly greater in plots under palmarosa+ than in the initial years. The wheat yield equivalent was significantly higher in plots under palmarosa+ followed by panicum and without VS. Thus, vegetation strips are recommended for wider adoption to reduce run‐off and soil loss and to increase crop yield. The long‐term goal is to achieve a palmarosa+ system (palmarosa as a vegetation strip along with organic amendments, farmyard manure, vermicompost and poultry manure) and weed mulch under minimum tillage.     

Dryland corn response to tillage and nitrogen fertilization. I. Growth‐yield‐N relationships

Abstract

Crop response to fertilizer nitrogen (N) is dependent upon tillage management. This study was conducted to determine how tillage rotation influences non‐irrigated crop growth, N uptake and yield. The effects of tillage rotation, N rate and N timing schedule on early season dry matter production and N uptake, ear leaf N concentration at silking, and yield of corn [Zea mays (L.) Pioneer 3378] were investigated at Painter, VA, on an Altavista loam (fine‐loamy, mixed, thermic Aquic Hapludult). In 1986, maximum yields achieved in the 6‐year continuous no till (NT) [5.82 Mg/ha] and first year no till (AT) [5.64 Mg/ha] were significantly greater than that of the 6‐year continuous conventional till (CT) [3.67 Mg/ha], but no yield differences were obtained in the drier 1987 season. A higher rate of N fertilizer was required to obtain maximum yield in the first year no till (168 kg N/ha) than in the NT (112 kg N/ha) during 1986. Early 1986 N uptake and growth response with and without N at planting increased in the order CT < AT = NT and AT < CT < NT, respectively, indicating greatest immobilization of soil N occurred in the newly established no till soil. Lack of differences in critical ear leaf N values developed for NT and CT in each year imply that plant norms developed for one tillage system may accurately assess N status of corn grown under different tillage practices.     

Effect of annual applications of pelletized dolomitic lime on soil chemical properties and grass productivity

Lime in pelletized form is potentially more convenient for farmers than ground limestone, as it can be applied using conventional fertilizer‐spreading equipment. Pelletized lime is intended to maintain an optimum soil pH when applied annually at a rate of 350 kg lime/ha/yr. Interactions between lime and N fertilizer rate were examined by applying 0, 75, 150, 225 and 300 kg N/ha/yr (as calcium ammonium nitrate) in combination with 0, 175, 350 and 525 kg pelletized dolomitic lime/ha/yr over 3 yr to a permanent grassland sward used for silage production in County Down, Northern Ireland. Equal rates of ground lime, from the same source as the pelletized lime, were applied as a comparison. Effects on soil chemical properties, grass dry matter (DM) yield and herbage nutrient removal were examined. Lime maintained or slightly increased the soil pH, particularly in the top 2.5 cm of the profile, but there was no difference in the performance of pelletized lime compared to ground lime in any of the parameters measured. Lime had no significant effect on grass DM yield or grass quality; however, there was a significant (P < 0.05) reduction in yield at the first cut, particularly in year 2, when the highest lime rate (525 kg lime/ha/yr) was applied in the absence of N fertilizer. The dolomitic nature of the lime (11% Mg) resulted in significant (P < 0.001) increases in soil and herbage magnesium levels, and this could be beneficial for reducing the incidence of grass tetany in grazing animals. The P content of the herbage was also significantly higher in plots receiving lime, which suggests that lime may have enhanced the mineralization of P or stimulated root growth.     

Effect of magnesium fertilization on yield and leaf composition of tomato plants

Tomato plants were grown for 2 years at 4 different rates of Mg fertilization on a Princeton loamy sand at pH 4.8 with 29 kg exchangeable Mg/ha. Calcareous limestone was used to provide a pH treatment in the second year. Magnesium deficiency symptoms were observed on plants grown on plots having ≤ 38 kg/ha NH₄OAC‐extractable Mg. Application of 56 kg Mg/ha corrected Mg deficiency and produced a significant increase in yield. Application of calcitic limestone also produced significant yield increases, but did not affect the development of Mg deficiency symptoms. Tomato yield was increased 27.9% by Mg application and 17.7% by lime application. Highest tomato yield was obtained with application of 112 kg Mg/ha. Symptoms of Mg deficiency were observed when the Mg concentration in recently mature leaf tissue was in the 0.30 to 0.32% range. Magnesium concentration in leaf tissue increased linearly with increasing Mg rate. Leaf Mg concentration at various growth stages of the tomato plant was variable depending on Mg treatment. Magnesium fertilization rate bad little effect on Ca or K leaf concentrations. Application of Calcltic limestone increased leaf tissue Ca and reduced leaf tissue Mg and Mn concentrations.     

Yield,forage quality,and nitrogen recovery rates of double‐cropped millet and ryegrass

Abstract

Pearl millet and annual ryegrass were continually doubled‐cropped on Olivier silt loam soil for seven years at six levels of N, applied as ammonium nitrate in three applications to millet and in two applications to ryegrass. Forage yields increased as N application rates increased. During seven years at the 0 and 448 kg/ha N rate, millet produced 35% and 95%, respectively, as much yield as it produced at the 800 kg/ha N rate, while comparable values for ryegrass were 19% and 83%. At 448 kg/ha of N the two grasses produced a combined yield of over 20 Mg/ha of dry forage per year. Ryegrass yields following millet were consistently lower than yields previously obtained at this site.

Nitrogen applications consistently increased concentrations of N, Ca, and Mg in both forage grasses, while effects on P and K were variable and S concentrations were unaffected. The amounts of all nutrients removed in the forages were increased as yields increased with N application rates. Nitrate‐N levels considered to be toxic to ruminant animals occurred only where N applications exceeded 170 kg/ha at any one time. In vitro digestibility of each grass was consistently increased by N applications.

The percentage of fertilizer N that was removed in the crops ranged from 66% to 68% for millet and from 35 to 52% for ryegrass as N applications increased up to 448 kg/ha. Residual ammonium and nitrate levels in the top 1.2 m of soil were not increased by N rates of 448 kg/ha or lower. At the 800 kg/ha N‐rate, the apparent N recovery rate decreased and residual ammonium and nitrate levels increased throughout the soil profile.     

Effect of lime,P, and Mg on growth and elemental concentrations of mugwort

Abstract

There is evidence that mugwort (Artemisia vulgaris L.) may have potential for use as a livestock forage. This study was undertaken to determine mugwort growth response to lime, P, and Mg, and their effect on elemental concentration of plant material.

Factorial combinations of 0, 5.6, and 11.2 mt lime/ha; 0, 112, and 224 kg P/ha; and 0, 224, and 448 kg Mg/ha were applied to low pH soil in greenhouse pots and planted to mugwort. In the absence of lime and Mg, growth was very poor. Lime was the most effective treatment in promoting mugwort growth. Growth response to Mg was greatest in the absence of lime, and response to P was dependent on lime and/or Mg application. Macronutrient concentrations of mugwort plants were considered adequate for use as forage for non‐lactating beef cows. Concentrations of several of the micronutrients were very high, especially at low lime and Mg. Copper was high at all treatments.     

Residual effects of sewage‐sludge application on plant and soil‐profile chemical composition

Abstract

Long‐term effects on plant and soil‐profile chemical composition imposed by a residential sewage sludge were studied on an Oxisol from Hawaii. Sludge was applied at 0, 45, 90, and 180 Mg/ha in 1983. An NPK‐fertilized treatment was included for comparison. Sudangrass (Sorghum bicolorL. Moench) was grown as a test crop in the 1983–84 and 1986–87 seasons. Soil samples for chemical analysis were taken in 1987 at three depths: 0–23 cm, 23–46 cm, and 46–69 cm.

Beneficial effects of sludge, measured 3 years after application (beginning of the 1986's planting), were evident by large yield increases on sludge‐amended soils relative to the unamended and the NPK‐fertilized soils. The first cutting produced approximately 5 Mg/ha of dry matter from the sludge treatments, regardless of rate, as compared with 3 and 1.5 Mg/ha from the NPK and the 0 treatments. Regrowths showed similar effect, though less dramatic; average yields were 2.6 Mg/ha with sludge and 1.6 Mg/ha without.

Heavy‐metal concentrations in plants were generally unaffected by sludge applications; probably because (i) heavy‐metal contents of the sludge were low, and (ii) soil pH was increased by sludge.

Remarkable increases in pH, exchangeable Ca and extractable P, and resultant decreases in exchangeable Al, in all three soil layers of sludge‐amended soils suggest that surface application of a low heavy‐metal sludge could serve to correct subsoil acidity and enhance subsoil P availability.     

Establishing native plants on newly‐constructed and older‐reclaimed sites along West Virginia highways

Many state highway departments in the USA must use native plants for revegetating roadsides. We conducted two field studies in West Virginia to assess native plant establishment under two different conditions. On newly‐constructed sites, native species were seeded alone or combined with non‐native species. On older roadsides, native species were seeded in disturbed existing vegetation. In the first study, we used four seed mixtures comprised of seeds of native and non‐native species, and two N‐P‐K fertilizer treatments at three newly‐constructed sites. Native, warm‐season grasses were slow to establish and only contributed 25 per cent cover in some plots after three years. Indiangrass (Sorghastrum nutans [L.] Nash), big bluestem (Andropogon gerardii Vitman), Brown‐Eyed Susan (Rudbeckia triloba L.), and wild senna (Cassia hebecarpa Fernald) were the only seeded native species found. Fertilizer at 150 kg ha⁻¹ of 10‐20‐10 showed little influence on increasing plant cover. In the second study, we disturbed three different‐aged established stands of vegetation composed of tall fescue (Festuca arundinacea Screb.) and crownvetch (Coronilla varia L.) by mowing, herbicide, or tillage, and native plants were seeded with and without fertilizer. Native cover was <10 per cent in all plots during the first year, but greatly increased by the second year to as much as 45 per cent in tilled plots, indicating that disturbance was necessary for natives to become important contributors within 2 years. Only switchgrass (Panicum virgatum L.), little bluestem (Andropogon scoparius Vitman), partridge pea (Chamaecrista fasciculate Michx.), and Brown‐Eyed Susan were observed in plots. Fertilizer at 300 kg ha⁻¹ of 10‐20‐10 did not increase native plant cover on these sites. Based on our results, introducing or increasing the cover of native species along roadsides requires (1) reducing competition from non‐native species, and (2) longer time periods for these slower‐establishing species to be observed. Copyright © 2008 John Wiley & Sons, Ltd.     

Role of continuous nitrogen fertilization on nutrient composition of leaves sampled at various stages of growth and on yield of yam (Dioscorea rotundata)

Abstract

White yam (Dioscorea rotundata cv. Olonko) was grown consecutively for three growing seasons, i.e. from February to October of 1975, 1976 and 1977, and treated with six levels of nitrogen, viz: 0, 40, 60, 120, 160 and 200 kg N/ha in the field. Leaf samples were taken at four stages of growth as follows: vegetative, tuber formation, tuber development and tuber maturation, and analyzed for NO₃‐N, P, K, Ca and Mg.

Increasing nitrogen fertilization consistently increased leaf‐NO₃‐N, particularly at the vegetative stages of growth, while no consistent trend was established for leaf‐P. Leaf‐K was increased at low rate of nitrogen fertilization during tuber formation and maturation whereas leaf‐Ca increased only at tuber maturation in the presence of higher rates of nitrogen fertilization. There was a marked increase in leaf‐Mg at all stages of growth when N treatment was increased to 200 kg N/ha. A positive correlation (r = 0.84???) was obtained for leaf‐K at the vegetative growth stage with tuber yield, while leaf‐Mg was positively correlated with tuber yield at vegetative (r = 0.46?), tuber formation (r = 0.50?) and tuber development (r = 0.67??) stages. All other elements were negatively correlated with yield at all stages of growth. Tuber yield was highest at the 200 kg N/ha treatment.     

Single vs. double cropping under two levels of fertilization with and without irrigation

Abstract

A corn‐small grain cropping sequence resulted in a greater total grain yield than corn or small grain alone or grain sorghum double cropped with small grain. Drought restricted yield responses to N, P and K in non‐irrigated plots but under irrigation grain yield for each cropping sequence was directly related to fertilizer applied. All fertilizer treatments increased soil acidity. Phosphorus and K applied at 26 and 50 kg/ha, respectively for each crop in the sequence maintained P and K levels in the soil. After three years, the high rate of fertilizer (87 and 166 kg/ha of P and K, respectively) resulted in greater soil P and K values than the low rate of fertilizer.