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Decontamination of soils by activation with acids and basesHardie, Ailsa Ghillaine 03 1900 (has links)
Thesis (MSc)--University of Stellenbosch, 2004. / ENGLISH ABSTRACT: New, more receptive surfaces can be generated in soils by a partial dissolution of existing,
crystalline solids followed by re-precipitation as poorly crystalline colloids with a larger
capacity to adsorb ionic and molecular contaminants. This priming process can be carried
out by treating the soil with strong acid or base and then neutral ising it again. The aim of
this study was to investigate the effectiveness of acid and base treatments in reducing
inorganic contaminant availability in different soil types.
The first study involved investigating the change in cation (cadmium[II], copper[II]) and
anion (phosphate) sorption of four different soils before and after priming. Hydrochloric
acid and KOH were used to adjust the pH of soils to below pH 2 or above pH 12 in the
dissolution stage of the priming treatment. After neutralisation it was found that base
priming resulted in an increase in metal cation adsorption in all the soils, most notably in the
sesquioxidic (increase from 19.5 to 73.5 mmol Cd.kg-1 soil) and kaolinitic soils (from 16.9
to 38.3 mmol Cd.kg-1 soil), whereas acid priming decreased it or had little effect on cation
sorption. However, acid priming increased anion sorption in all soil types, to a greater extent
than base priming, most notably in the organic soil (from 6.3 to 14.7 mmol P04.kg-1 soil).
This can be attributed to the differences in the nature of the precipitate (more aluminous or
alumino-siliceous) depending on whether the dissolution was carried out in acid or basic
conditions, and the final pH of the soil solution, as the hydroxyaluminium and
hydroxyaluminosilicate precipitates which form are known to enhance pH-dependent
sorption of metals.
In the second study, the soil was suspended in Cd or Cu solutions and then the pH was
adjusted to below 2 or above 12 using HCI or KOH. After 5 days of shaking the pH was
adjusted to a neutral pH again. The availability of the Cd and Cu was determined at each of
the stages in the treatment, and it was found that both the acid and base treatments were
effective in removing Cu from solution, whereas only the base treatment was effective in
removing Cd. Determinations were also carried out using H2S04 and Ca(OH)2 and it was
found that they were equally effective. It can be proposed that this acid-base pair would be of most practical importance as the salt generated is gypsum which is generally considered
benign, and can actually help to improve the soil structure.
Activation of soils by acid or base conditioning could have some useful applications in
decontaminating soils or decreasing the mobility of inorganic contaminants in soils. Primed
soils could also be used as cheap absorbents for decontaminating water. / AFRIKAANSE OPSOMMING: DEKONT AMINERING VAN GROND DEUR AKTIVlERING MET SURE EN
BASISE
Nuwe, meer ontvanklike oppervlakke kan in gronde gegenereer word deur middel van
gedeeltelike oplossing van bestaande, kristallyne vaste stowwe gevolg deur herpresipitasie
as swak kristallyne kolloïede met 'n groter kapasiteit om ioniese en molekulêre
kontaminante te adsorbeer. Hierdie behandelingsproses kan uitgevoer word deur die grond
met sterk suur of basis te behandel en dit daarna te neutraliseer. Die doel van hierdie studie
was om die effektiwiteit van suur- of basisbehandelings om anorganiese kontaminante te
verminder, in verskillende grond tipes te ondersoek.
Die eerste studie het die ondersoek na die verandering in katioon- (kadmium[II], koper[lI])
en anioon- sorpsie (fosfaat) van vier verskillende gronde voor en na suur of basis
voorbehandeling behels. Soutsuur en KOH was gebruik om die pH van die gronde tot onder
pH 2 of bo pH 12 aan te pas gedurende die oplosstadium van die behandelingsproses. Na
neutralisasie is dit gevind dat basis voorbehandeling tot 'n toename in metaal
katioonadsorpsie in al die gronde gelei het, en dit was veral waarneembaar in die
seskwioksied (toename van 19.5 tot 73.5 mmol Cd.kg" grond) en kaolinitiese (van 16.9 tot
38.3 mmol Cd.kg-1 grond) gronde, terwyl suur voorbehandeling dit verlaag het of 'n klein
effek op katioonsorpsie gehad het. Suur voorbehandeling, egter, het anioonsorpsie in al die
gronde verhoog, tot 'n groter mate as basis voorbehandeling, veral in die organiese grond
(van 6.3 tot 14.7 mmol fosfaat.kg' grond). Dit kan toegeskryf word aan die verskille in die
aard van die neerslag wat meer alurninium- of alurniniumsilika-ryk kan wees afhangede of
die oplossing uitgevoer was in suur of basis kondisies, en ook die finale pH van die
grondoplossing omdat die hidroksi-aluminium en hidroksi-aluminiumsilikaat presipitate wat
vorm bekend daarvoor is om pH-afhanklike sorpsie van metale te bevorder.
In die tweede studie, was die grond in Cd- of Cu-oplossings gesuspendeer en die pH was
aangepas tot onder 2 of bo 12 met HCI of KOH. Na vyf dae van skud was die pH weer
aangepas tot by neutraal. Die beskikbaarheid van Cd en Cu was bepaal by elke stadium in
die behandeling, en dit is gevind dat beide suur- en basisbehandeling meer effektief was in
die verwydering van Cu uit oplossing, terwyl slegs die basisbehandeling effektief was in die verwydering van Cd. Bepalings was ook uitgevoer met die gebruik van H2S04 en Ca(OH)2
en dit is gevind dat dit net so doeltreffend was soos HCI en KOH. Dit kan voorgestel word
dat hierdie suur-basis paar in die praktyk belangriker sal wees omdat die sout wat
gegenereer word, nl. gips, as 'n gunstige sout beskou word.
Aktivering van grond deur suur- of basis-kondisionering kan sekere bruikbare toepassings in
die dekontaminering van gronde hê of dit kan gebruik word om die mobiliteit van
anorganiese kontaminante te verlaag. Suur of basis voorbehandelde gronde kan ook gebruik
word as goedkoop absorbante vir die dekontaminering van water.
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Replacement of the natural bases of the exchange complexes of soil with known cations, and the effect of such soil upon the solubility of phosphate fertilizers in the presence of varying amounts of calcium carbonate and potassium chlorideBenne, Erwin John January 1931 (has links)
Typescript, etc.
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Organo-mineral associations in soilsTurchenek, Larry William January 1975 (has links)
xvii, 275 leaves : ill., tables, photos ; 26 cm. / Title page, contents and abstract only. The complete thesis in print form is available from the University Library. / Thesis (Ph.D.)--University of Adelaide, Dept. of Agricultural Biochemistry and Soil Science, 1976
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Organo-mineral associations in soils.Turchenek, Larry William. January 1975 (has links) (PDF)
Thesis (Ph.D.) -- University of Adelaide, Dept. of Agricultural Biochemistry and Soil Science, 1976.
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Chemistry of the soils of the Lismore district, New South Wales /Tucker, Bruce Mollet. January 1957 (has links) (PDF)
Thesis (M.Sc.) --University of Adelaide, 1957. / Typewritten copy.
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Replacement of the natural bases of the exchange complexes of soil with known cations, and the effect of such soil upon the solubility of phosphate fertilizers in the presence of varying amounts of calcium carbonate and potassium chlorideBenne, Erwin John January 1931 (has links)
Typescript, etc.
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Some aspects of the movements of ions in soilsGraham-Bryce, I. J. January 1961 (has links)
No description available.
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Studies in soil chemistry and forest nutritionRaupach, Maxwell January 1977 (has links)
1v. (various paging) : / Title page, contents and abstract only. The complete thesis in print form is available from the University Library. / Thesis (D.Sc.1979)--University of Adelaide, Dept. of Physical and Inorganic Chemistry, 1979
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THE CHEMICAL BEHAVIOR OF CERTAIN SYNTHETIC METAL CHELATES IN SOILSElgala, Abdelmonem Mohamed Abdalla, 1935- January 1966 (has links)
No description available.
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Soluble constituents and ion exchange reactions of Champlain sea sediments.Laventure, Reginald S. January 1964 (has links)
The Champlain Sea sediments are the parent materials of some of the most important agricultural soils of Quebec. They contain a high proportion of clay-size particles which are primary minerals derived from igneous and metamorphic rocks. The mineralogy and mode of deposition give rise to unusual properties. The physical properties of these sediments have stimulated many studies of their geotechnical properties but only limited information is available for chemical properties. [...]
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