Browsing by Author "Gurung, Shivaraj"

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    Aluminium interaction with organic matter and fluoride during soil development in oxidised mine waste : a thesis presented in partial fulfilment of the requirements for the degree of Master of Science in Soil Science, Massey University
    (Massey University, 1994) Gurung, Shivaraj
    Significant differences in plant growth response between unmodified waste rock (UWR) and modified (treated with lime and phosphate fertilizers) waste rock (MWR) with topsoil treatments during the first two years of a field trial conducted by Gregg & Stewart (1986; 1987) indicated that Al toxicity was affecting root growth in the UWR. By the end of three years of field trial there was no significant difference in dry matter yield between the MWR and UWR with topsoil treatments indicating possible amelioration of Al toxicity (Gregg et al., 1990). The objective of this study was to measure different forms of Al and F in the soil and waste rock at the end of the third year of field trial and to determine the mechanism of amelioration of Al toxicity in these soils. Results of this study revealed that there was a significant 2-fold increase in organic-Al (Al-OM) at the UWR interface (B) compared with the waste rock at depth (C) by the end of three year period of soil development. Organic matter decomposition in the topsoil during three years and movement of the soluble organic ligands to UWR interface (B) resulted in conversion of phytotoxic soil solution Al into non-toxic Al-OM forms by complexation with organic ligands in leachates accumulated in the UWR interface. Total soluble F was consistently high in the UWR profile with a mean value ranging from 1.0 to 1.9 µ,g g·1 . Liming has reduced the F level to 0.3-0.4 µ,g g·1 in the MWR interface (B) and 0.4-0.5 µ,g g·1 in the topsoil (A). The waste rock at depth (C) had mean F values in the range 1.2-1.9 µ,g g·1 . High levels of F in the waste rocks could have also ameliorated Al toxicity in the UWR by formation of non-phytotoxic soluble AlF complexes. This was considered to be another possible reason for no significant differences in the pasture yields between UWR and MWR plots at the end of the third year of trial. The mean soil pH(H20 ) for the UWR was 5.1 and liming has raised it by about 1 unit in the MWR. The corresponding pH(0.01 M CaCl2) values were 0.4-0.8 units less than the pH in water. The 0.02 M CaC12-extractable solution Al (Al-Ca) and 1 M KCl­- extractable exchangeable+ solution Al (Al-K) have remained high in UWR soil solution irrespective of different depths of topsoil treatments. The Al-Ca and Al-K ranged from 16.7 to 20.5 µ,g g·1 and 261 to 339 µ,g g·1 respectively in the UWR interface (B). The Al-Ca and Al-Kin waste rock at depth (C) remained at 16.8-22.9 µ,g g·1 and 238-369 µ,g g·1 respectively. Modifications have lowered both Al-Ca and Al-K to 0.8-2.7 µ,g g·1 and 35-66 µ,g g·1 respectively in the MWR interface (B). Topsoil Al-Ca and Al-K were not significantly different between UWR and MWR and the values for these two forms of Al ranged from 0.6 to 6.0 µ,g g·1 and 32-87 µ,g g·1 respectively at the end of the field trial. Normal plant growth response in the UWR in spite of high levels of Al-Ca and Al-K indicated that 0.02 M CaC12 and 1 M KCl extractants are not good indicators of phytotoxicity as reported in literature because these extractants may be extracting a substantial proportion of non-phytotoxic species of Al.
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    Characterisation and amelioration of low pH conditions in pyritic mine pitwall materials, Martha Mine, Waihi, New Zealand : a thesis submitted in partial fulfilment of the requirements for the degree of Doctor of Philosophy in Soil Science, Massey University
    (Massey University, 1998) Gurung, Shivaraj; Gurung, Shivaraj
    The objective of this thesis was to research the processes associated with the generation of low pH conditions in pitwall rock material at Martha Mine, Waihi, and evaluate the ameliorating effectiveness of some selected acid neutralising materials with an aim to create suitable plant growth media. Approximately 25% of the current pitwall area is affected by pyrite oxidation, resulting in the formation of acid mine drainage (AMD) which limits long-term establishment of vegetation. The results of this study showed that slope gradient, variable cover material distribution and persistent rill and sheet erosion on the pitwall are some of the physical characteristics restricting plant establishment. Weathered cover materials varied in depth from 5 mm on the upper slopes to > 300 mm in the lower colluvial section of the pitwall. The uneven distribution of pyrite mineralisation has resulted in microenvironments of "acid pockets" in oxidised parts of the pitwall. The fresh pyritic rock had a near neutral pH while the strongly weathered materials generally had pH < 3.0. Based on the total sulphide S content (2.51%). the fresh rock had a net acid producing potential (NAPP) of 51 kg CaCO3 t-1. Weathered material still contained significant amounts of sulphide S but because of negative neutralisation potential (NP), it had a higher NAPP of 82 kg CaCO3 t-1. Kinetic net acid generation (NAG) test revealed that the fresh rock, when exposed, had a lag-period of 22 weeks for the onset of biochemical oxidation. However, the degree of pyrite liberation from the host rock materials is likely to effect the lag-period. The effect of progressive weathering and oxidation was to cause major losses in base cations except for K, which showed an anomalous enrichment, due to incorporation into clays and jarosite-type minerals. Weathering also caused relative enrichment in Ba and As contents of the pitwall materials. Run-off water collected from the bottom of the pitwall had the characteristic AMD composition of low pH and high dissolved metal concentrations. The spatial variation of pH of the weathered pitwall rock in the study area was in the range 2.0-4.6 while EC varied from 1.9 to 4.3 dS m-1. The study area generally contained high concentrations of soluble Fe (2506-5758 mg kg-1), Mn (203-635 mg kg-1), exchangeable-Al (4.8-10.8 cmolc kg-1), SO4 2- (1650-3400 mg kg-1) and acidity (121-668 kg CaCO3 t-1). Overall, NAPP distribution varied from 35 to 143 kg CaCO3 t-1. A buffer curve lime requirement (LRBuffer) to raise the pH of the weathered pitwall rock material to 6 (29 kg CaCO3 t-1) amounted only to 35% of the acid base accounting (ABA) value of 82 kg CaCO3 t-1. This suggested that the LRBuffer only accounted for the acid generated from dissolution of hydroxide precipitates of Fe and Al. It was found that in order to account for the NAPP of the pitwall material, it was important that the lime required to neutralise the potential acidity (LRNAPP) be added to the LRBuffer to give the total lime requirement (LRTotal) for long-term control of acid generation. A 90 days incubation assessment of selected neutralising materials (limestone, LST; dolomite, DOL; reactive phosphate rock, RPR; fluidised bed boiler ash, FBA) indicated that LST, DOL and FBA were similar in attaining the target pH of 6 at a carbonate content equivalent rate (CER) of 30 kg CaCO3 t-1. The RPR did not raise the pH > 4.5 even at CER of 50 kg CaCO3 t-1 but it was equally effective in overall reduction of EC, SO4 2-, acidity, Fe, Mn and Al in the incubated pitwall rock material. The coarser the grain size, the less reactive the neutralising material was, mainly due to an armouring effect from the Fe and Al hydroxide coatings. While fine-grained material provided quick neutralisation of acid, long-term buffering of the pH may not be possible due to continued generation of acid as more pyrite grains are liberated for oxidation. On the other hand, materials like RPR and coarse LST may provide slow release neutralisation from repetitive dissolution of hydroxide coatings when reacidification occurs. Results of the column experiments on the assessment of ameliorative effectiveness of neutralising materials on leachate quality and subsurface acidity indicated that although application of amendments significantly raised the pH at 0-60 mm column depth, the leachate pH remained below 2.5 throughout the 12 weeks leaching cycle. The concentrations of EC, SO4 2-, acidity, Fe, Mn and Al were however, significantly reduced both in the leachate and subsurface column sections. At depth > 60 mm, the leached columns remained acidic irrespective of treatments. Broadcasted and incorporated methods of application of neutralising material amendments showed similar trends in effectiveness of amelioration. However, the overall ameliorative effectiveness was significantly better with incorporated method of amendments. Surface application of a shallow depth of topsoil (TS) and incorporation of bactericide ProMac (PM) were found effective in the amelioration of low pH conditions of the pitwall rock material by raising pH and significantly reducing sub-surface concentrations of SO4 2-, acidity, Fe, Mn and Al. The amended columns however, still produced effluent pH of <2.5. The overall results from the study indicated that with detailed on-site characterisation and using laboratory studies to formulate appropriate combinations of neutralising materials, the pyritic pitwall rock materials could be suitably modified for plant growth. In practice, the placement of the amendments on the pitwall remains an engineering challenge.