Thesis (Ph. D.)--University of Wisconsin, 1967. / Typescript. Vita. eContent provider-neutral record in process. Description based on print version record. Includes bibliography.

Thesis (Ph. D.)--University of Wisconsin--Madison, 1966. / Typescript. Vita. Includes facsimile of one published journal article and texts for two articles to be submitted to journals, all by the author and M.L. Jackson. Description based on print version record. Includes bibliographical references (leaves 116-128).

Thesis (M.S.)--Oregon State University, 2007. / Printout. Includes bibliographical references (leaves 89-95). Also available on the World Wide Web.

Infrared spectroscopy was used to show that the arsenate anion is adsorbed on the surface of synthetically prepared goethite, replacing two singly coordinated (A-type) surface OH groups. In this respect, arsenate is analogous to phosphate, but its larger size causes it to interact more strongly with other OH groups that remain on the surface. This has suggested an alternative infrared band assignment for these OG groups. Potentiometric titrations performed on 'CO<SUB>2</SUB>'-free goethite gave a value for the point of zero charge (p.z.c.) of 9.15. The p.z.c. shifted to more acid values for phosphate- and arsenate-treated goethite indicating an increased negative surface charge. For sulphate-treated goethite the positive surface charge increased slightly. The results were interpreted as indicating that phosphate and arsenate were adsorbed by a chemisorption (ligand-exchange) mechanism. The exact nature of the sulphate interaction was still unclear. Solution studies on the goethite-aqueous solution interface demonstrated the adsorption of arsenate by a binuclear bridging mechanism, confirming the findings from the infrared study. The results indicated a 2:1 stoichiometry between ligands exchanged and arsenate adsorbed over the pH range 4-10. No such stoichiometry was observed for sulphate adsorption though the reaction between sulphate and goethite consumed protons (i.e. released hydroxyl). A brief study to ascertain the effect of certain competitors on arsenate adsorption was performed. Results showed considerable reduction in arsenate adsorption when vanadate ions were added simultaneously with arsenate to goethite-aqueous electrolyte suspensions. The results also indicated that goethite previously coated with small quantities of humic acid reduced arsenate adsorption. The presence of sulphate in solution at up to five times the concentration of arsenate had no effect on arsenate adsorption over the pH range 5 to 9.

1. Accurate and reproducible methods for the determination of N and acid- extractable P in soils are described. The variations in N, P, and K found by intensive sampling of three different soil types are presented. 3. Suggestions for the adequate sampling of soils for various purposes arc given. 4. A study is presented of the preparative stages in leaf analysis (washing, drying, grinding and storage) as applied to citrus and pineapple leaf material. Likely errors are pointed out and procedures whereby these may be minimised are described. 5. A reliable wet-ashing procedure for obtaining leaf solutions is described. 6. Accurate and reproducible methods for the determination of total N, P,. K, Ca, Mg, Na, Fe, Mn, Zn and Cu in citrus and pineapple leaves are presented. 7. It is shown that diurnal variations in nutrient concentrations occur in citrus and pineapple leaves. 8. The variations in N, P, K, Ca, Mg, Na, Fe, Mn, Zn and Cu, occurring from tree to tree in 3 different Navel orange blocks are presented. It is shown that if all these elements are to be represented . to within 10% of the mean values on a 19 : 1 probability level, all the trees in the blocks would have to be sampled. Reasonable sampling procedures for various purposes are suggested. 9. The variations in N, P, K, Ca, Mg, Fe, Mn, Zn and Cu, occurring in 3 different Cayenne pineapple plantations are presented and described. Suitable sampling procedures are suggested.

Vegetation and soils were evaluated on a black-tailed prairie dog (Cynomys ludovicianus) colony and adjacent non-disturbed mixed-grass prairie in central South Dakota. The study’s objectives were 1) determine differences in plant species diversity and richness, and selected soil quality parameters between prairie dog colonies and adjacent non-disturbed sites, and 2) evaluate impacts of prairie dogs on water infiltration rates. Three soil series were evaluated representing three ecological sites (Opal, Cabba, and Wayden). Plant species richness was higher on the Control on Opal soils, while being lower on the Control on Cabba soils. Lower soil pH and higher nitrate concentrations were found on the prairie dog town for Opal and Cabba soils near the soil surface, close to the prairie dog mounds. These findings show prairie dog impacts on soil parameters can vary across different soil types, which can affect the diversity and richness of vegetative communities within prairie dog colonies.

The adsorption reaction of zinc onto prochlorite, pyroxene, and biotite minerals, from dilute solution (water) was studied under isothermal conditions by agitated nonflow experiment method. The equilibrium concentration of zinc in the solution was determined both by radioactive tracer technique and adsorption spectrophotometer methods. The data were collected at three temperatures. The data were treated by the equation: ∂θ/∂t = kl(1-θ)C-k-1θ where θ is the fraction of total surface coverage and C is the equilibrium concentration of zinc in solution, k1 and k-1 are the rate constants for the adsorption and reverse process and t is the time of reaction. The specific rate constant for the adsorption reaction (k1) depends on the nature of the mineral and mineral particle fraction. The k1 increases with rise in temperature. The values for the desorption rate constant (k-1) are small, indicating that zinc ions are preferentially adsorbed over other exchangeable ions in the system. The activation energy for the sorption process lay between 3 to 6 kcals/mole , eliminating chemical adsorption. The activation energy indicates the physical process of diffusion as the mechanism cont rolling step in the present study. The positive standard entropy of activation (ΔSŦ) is related to the change in the volume of activation complex (θŦ) during the course of reaction. The monolayer capacities for the three minerals and mineral fractions were evaluated. The percent of the surface area occupied by the adsorbed zinc ion was about 50 percent, 65 percent and 66 percent for prochlorite, pyroxene and biotite, respectively . This suggests that zinc is adsorbed on certain specific sites.The monolayer capacities increase as the temperature increases. The change in the standard free energy of adsorption, -Δ°G , with the increased fraction of surface coverage allows speculation that : The sites are energetically heterogenous. There is mutual repulsion of adsorbed zinc ions at higher surface coverage. The data show that zinc adsorption onto the minerals used in the present study is exchange adsorption. The initial adsorption plateau in the case of prochlorite and pyroxene is described as a result of exchange of solution zinc for weakly adsorbed sodium. The change in the nature of the curve beyond this region is speculated to the progressive exchange of other cations. The data for biotite are not conclusive and need further study. It appears that exchange adsorption is a step wise process and more than one plateau may be obtained if t he system is allowed to reach its ultimate equilibrium where all the exchange sites are completely saturated by the adsorbate. The small differential heat of adsorption () confirms the contention that the process is simply an exchange adsorption in the systems studied.

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No description available.

The South Burnett region of Queensland is Australia's most important rainfed peanut (Arachis hypogea L.) production area. It also produces a considerable amount of cereal and grain legume crops. The cropping soils of the region are red, acid to neutral, clay loams that are classified as Ferrosols (Australian Soil Classification). Over 50 years of cropping on these soils has resulted in severe depletion of nutrient reserves, particularly potassium (K). In addition, the remaining K is predominantly confined to the surface 10 or 15cm of the soil profile, a feature commonly refered to as nutrient stratification. Dry periods during the summer cropping season are common due to the highly variable, summer-dominant rainfall pattern of the South Burnett. As topsoil dries out, crops forage for moisture and nutrients from lower in the soil profile where K reserves are smaller. It is therefore suspected that the combination of dry periods and stratified K reserves have resulted in an increasing incidence of K deficiency symptoms in summer crops. To investigate these issues, K relations of Ferrosols of the South Burnett were studied using soils from two representative sites. The pools of soil K that are important to crop growth in Ferrosols, and their interaction was examined through fractionation of soil K pools, and determination of quantity/intensity relationships, charge characteristics and clay mineralogy, and a leaching column study. A rapid K uptake period was identified for peanut and the effect of profile distribution and soil moisture during this period on K accessibility was studied in a divided column experiment. Finally, on-farm trials were used to evaluate commercial-scale options for improving K distribution in field profiles. It was found that the immediately available exchangeable K pool in these soils was the most important source of soil K, and was poorly buffered by slowly available non-exchangeable K. However the leaching column study revealed that K was preferentially adsorbed onto soil cation exchange sites, displacing calcium (Ca) and magnesium (Mg) ions, and therefore was not susceptible to vertical movement within the soil profile. These observations helped to explain the development of stratified K profiles in these soil types. Peanut (cv. Streeton) was found to take up most of its K requirement between 25-70 days after planting. The divided column study showed that profile distribution, and topsoil iv moisture content during this rapid K uptake period, were able to affect the ability of peanut plants to access K. Plants that grew in low K soil, or where soil was dry at the site of K supply, had reduced access to K. However, improving access to K did not result in improved growth, but rather in a significant reduction in dry matter (DM) production, apparently due to interference in the availability of other nutrients, possibly phosphorus (P), magnesium (Mg) or boron (B). Field studies showed that application of K and profile inversion improved K uptake and DM production of various crop species. However, in most instances improved K uptake and DM production was not reflected in increased yield. It was suggested that a combination of agronomic factors, seasonal conditions and crop type prevented the expression of yield responses to improved K nutrition and these influences need to be understood. The findings of this project have important consequences for nutrition of crops grown on Ferrosols in the South Burnett region. Surface applied K cannot be expected to increase exchangeable K in the subsoil unless it is incorporated to depth. Similarly, band applied K will remain close to the site of application as a result of only limited vertical or lateral movement. This may affect the ability of roots to access band applied K. The ability of surface applied K to displace Ca and Mg from soil exchange sites may have negative implications for the Ca nutrition of developing peanut pods. On the other hand, it could present an opportunity for the movement of Ca into deeper soil layers to address the amelioration of acid subsoils. The unexplained negative responses to potassium chloride application and apparent effect on P, Mg or B nutrition need to be investigated.