Reduced Inorganic Sulfur Speciation in Drain Sediments from Acid Sulfate Soil Landscapes

2006 ◽  
Vol 40 (3) ◽  
pp. 888-893 ◽  
Author(s):  
Edward D. Burton ◽  
Richard T. Bush ◽  
Leigh A. Sullivan
Keyword(s):  
Acid Sulfate Soil ◽  
Acid Sulfate ◽  
Inorganic Sulfur ◽  
Sulfur Speciation

Assessment of peroxide oxidation for acid sulfate soil analysis. 1. Reduced inorganic sulfur

Soil Research ◽  
2002 ◽  
Vol 40 (3) ◽  
pp. 433 ◽  
Author(s):  
Nicholas J. Ward ◽  
Leigh A. Sullivan ◽  
Richard T. Bush ◽  
Chuxia Lin
Keyword(s):  
Soil Analysis ◽  
Total Carbon ◽  
Peroxide Oxidation ◽  
Acid Sulfate Soil ◽  
Acid Sulfate ◽  
Total Carbon Content ◽  
Inorganic Sulfur ◽  
Sulfur Determination ◽  
Pyritic Sulfur ◽  
Large Reserve

The reduced inorganic sulfur fraction of 4 acid sulfate soil (ASS) materials was quantified using a variety of peroxide oxidation procedures. The temperature and duration of the peroxide oxidation were found to markedly affect the peroxide oxidisable sulfur determination. For 3 ASS materials with low total carbon content (i.e. <2.5% C), peroxide oxidisable sulfur underestimated the reduced inorganic sulfur fraction, with the peroxide oxidisable sulfur determinations being as low as 42% of those determined using chromium reducible sulfur technique. The precipitation of jarosite during peroxide oxidation was a major factor contributing to the underestimation of reduced inorganic sulfur in these materials. Apparent losses of sulfur of approximately 25% on average occurred during peroxide oxidation budget accounting; this also contributed towards the observed underestimation of reduced inorganic sulfur. It is most likely that these unaccounted losses are due to atmospheric losses of sulfur. In a peat ASS, one of the peroxide oxidation methods overestimated the reduced inorganic sulfur fraction and was attributed to the release of a large reserve of organic sulfur in this material by the peroxide. This study shows the peroxide oxidation methods examined here are subject to substantial interferences. Consequently these peroxide oxidation methods are unable to reliably provide accurate measurements of the reduced inorganic sulfur fraction in ASS materials. pyritic sulfur, peroxide oxidisable sulfur, chromium reducible sulfur, jarosite, sulfur budget.

The response of partially oxidised acid sulfate soil materials to anoxia

Soil Research ◽  
2004 ◽  
Vol 42 (6) ◽  
pp. 515 ◽  
Author(s):  
Nicholas J. Ward ◽  
Leigh A. Sullivan ◽  
Richard T. Bush
Keyword(s):  
Organic Matter ◽  
Sulfide Oxidation ◽  
Management Strategies ◽  
Oxidation Products ◽  
Acid Sulfate Soil ◽  
Acid Sulfate ◽  
Anoxic Conditions ◽  
Inorganic Sulfur

Four acid sulfate soil (ASS) materials were subjected to anoxia after varying periods of oxidation to determine the geochemical response of these types of soils to flooding. The response of the partially oxidised ASS materials to the exclusion of oxygen was variable. The rate of sulfide oxidation, acidification, and the production of soluble oxidation products such as sulfate, iron, and aluminium generally decreased markedly when subjected to anoxia. However, especially in the highly acidic ASS materials (i.e. pH <3.5), sulfide oxidation and acidification generally continued (albeit at much slower rates), most probably due to oxidation by Fe3+. Rapid sulfide re-formation occurred in the peat ASS material that had been oxidised for 63 days, with 0.47% reduced inorganic sulfur (SCR) formed over 60 days of anoxia. This substantial sulfide re-formation was accompanied by only a slight increase in pH. Minimal sulfide re-formation occurred in 2 of the ASS materials when placed in anoxic conditions, most likely due to a lack of readily available organic matter in these materials. The results show that the imposition of anoxic conditions on partially oxidised ASS materials is generally effective in decreasing the rates of further sulfide oxidation, acidification, and the production of soluble sulfide oxidation products. Biogeochemical sulfide formation consumes acidity; however, sulfide re-formation was ineffective in reversing acidification under the conditions of this experiment. The results indicate that the treatment of sites containing actual ASS materials by management strategies relying on oxygen exclusion need to be accompanied by other strategies that include acidty neutralisation or containment.

A modified chromium-reducible sulfur method for reduced inorganic sulfur: optimum reaction time for acid sulfate soil

Soil Research ◽  
2000 ◽  
Vol 38 (3) ◽  
pp. 729 ◽  
Author(s):  
L. A. Sullivan ◽  
R. T. Bush ◽  
D. M. McConchie
Keyword(s):  
Reaction Time ◽  
Rock Sample ◽  
Reaction Times ◽  
Acid Sulfate Soil ◽  
Acid Sulfate ◽  
Inorganic Sulfur ◽  
Modified Method ◽  
Optimum Reaction

Reaction times for 16 acid sulfate soil materials analysed using a modified chromium-reducible sulfur method varied between 10 and 15 min, regardless of whether the samples had been dried and ground prior to analysis or were analysed without pretreatment. The reaction time for a ground (<63 mm) pyritic rock sample was 20 min. An optimum reaction time of 20 min is recommended for analysing acid sulfate soil using the modified method; this reaction time is much less than the 1 h reaction time used in previous methods.

PEUBAH KUALITAS AIR YANG MEMPENGARUHI PERTUMBUHAN RUMPUT LAUT (Gracilaria verrucosa) DI TAMBAK TANAH SULFAT MASAM KECAMATAN ANGKONA KABUPATEN LUWU TIMUR PROVINSI SULAWESI SELATAN

2009 ◽  
Vol 4 (1) ◽  
pp. 125
Author(s):  
Akhmad Mustafa ◽  
Rachmansyah Rachmansyah ◽  
Dody Dharmawan Trijuno ◽  
Ruslaini Ruslaini
Keyword(s):  
Water Quality ◽  
Growth Rate ◽  
Ammonium Phosphate ◽  
Gracilaria Verrucosa ◽  
Acid Sulfate Soils ◽  
Acid Sulfate Soil ◽  
Acid Sulfate ◽  
Independent Variables ◽  
Water Quality Variables ◽  
Sulfate Soils

Rumput laut (Gracilaria verrucosa) telah dibudidayakan di tambak tanah sulfat masam dengan kualitas dan kuantitas produksi yang relatif tinggi. Oleh karena itu, dilakukan penelitian yang bertujuan untuk mengetahui peubah kualitas air yang mempengaruhi laju pertumbuhan rumput laut di tambak tanah sulfat masam Kecamatan Angkona Kabupaten Luwu Timur Provinsi Sulawesi Selatan. Pemeliharaan rumput laut dilakukan di 30 petak tambak  terpilih selama 6 minggu. Bibit rumput laut dengan bobot 100 g basah ditebar dalam hapa berukuran 1,0 m x 1,0 m x 1,2 m. Peubah tidak bebas yang diamati adalah laju pertumbuhan relatif, sedangkan peubah bebas adalah peubah kualitas air yang meliputi: intensitas cahaya, salinitas, suhu, pH, karbondioksida, nitrat, amonium, fosfat, dan besi. Analisis regresi berganda digunakan untuk menentukan peubah bebas yang dapat digunakan untuk memprediksi peubah tidak bebas. Hasil penelitian menunjukkan bahwa laju pertumbuhan relatif rumput laut di tambak tanah sulfat masam berkisar antara 1,52% dan 3,63%/hari dengan rata-rata 2,88% ± 0,56%/hari. Di antara 9 peubah kualitas air yang diamati ternyata hanya 5 peubah kualitas air yaitu: nitrat, salinitas, amonium, besi, dan fosfat yang mempengaruhi pertumbuhan rumput laut secara nyata. Untuk meningkatkan pertumbuhan rumput laut di tambak tanah sulfat masam Kecamatan Angkona Kabupaten Luwu Timur dapat dilakukan dengan pemberian pupuk yang mengandung nitrogen untuk meningkatkan kandungan amonium dan nitrat serta pemberian pupuk yang mengandung fosfor untuk meningkatkan kandungan fosfat sampai pada nilai tertentu, melakukan remediasi untuk menurunkan kandungan besi serta memelihara rumput laut pada salinitas air yang lebih tinggi, tetapi tidak melebihi 30 ppt.Seaweed (Gracilaria verrucosa) has been cultivated in acid sulfate soil-affected ponds with relatively high quality and quantity of seaweed production. A research has been conducted to study water quality variables that influence the growth of seaweed in acid sulfate soil-affected ponds of Angkona Sub-district East Luwu Regency South Sulawesi Province. Cultivation of seaweed was done for six weeks in 30 selected brackishwater ponds. Seeds of seaweed with weight of 100 g were stocked in hapa sized 1.0 m x 1.0 m x 1.2 m. Dependent variable that was observed was specific growth rate, whereas independent variables were water quality variables including light intensity, salinity, temperature, pH, carbondioxide, nitrate, ammonium, phosphate, and iron. Analyses of multiple regressions were used to determine the independent variables which could be used to predict the dependent variable. Research result indicated that relative growth rate of seaweed in acid sulfate soils-affected brackishwater ponds ranged from 1.52% to 3.63%/day with 2.88% ± 0.56%/day in average. Among nine observed water quality variables, only five variables namely: nitrate, salinity, ammonium, phosphate and iron influence significantly on the growth of seaweed in acid sulfate soils-affected brackishwater ponds. The growth of seaweed in acid sulfate soils-affected brackishwater ponds of Angkona District East Luwu Regency, can be improved by using nitrogen-based fertilizers to increase ammonium and nitrate contents and also fertilizers which contain phosphorus to improve phosphate content to a certain level. Pond remediation to decrease iron content and also rearing seaweed at higher salinity (but less than 30 ppt) can also be alternatives to increase the growth of seaweed.

Ammonium nitrogen uptake by rice grown in acid sulfate soil under controlled redox conditions

1996 ◽  
Vol 46 (2) ◽  
pp. 103-109 ◽  
Author(s):  
A. Jugsujinda ◽  
J. Prasittikhet ◽  
R. D. DeLaune ◽  
C. W. Lindau ◽  
R. P. Gambrell
Keyword(s):  
Nitrogen Uptake ◽  
Ammonium Nitrogen ◽  
Redox Conditions ◽  
Acid Sulfate Soil ◽  
Acid Sulfate

Ca-Al-Containing Slag As an Advanced Fenton System for the Remediation of Acid Sulfate Soil

2021 ◽  
Author(s):  
Jiachen Zeng ◽  
Bo Feng ◽  
De Wei ◽  
Runli Tao ◽  
Baolin Shi ◽  
...  
Keyword(s):  
Acid Sulfate Soil ◽  
Acid Sulfate ◽  
Fenton System

Iron and sulfur cycling in acid sulfate soil wetlands under dynamic redox conditions: A review

Chemosphere ◽  
2018 ◽  
Vol 197 ◽  
pp. 803-816 ◽  
Author(s):  
Niloofar Karimian ◽  
Scott G. Johnston ◽  
Edward D. Burton
Keyword(s):  
Redox Conditions ◽  
Sulfur Cycling ◽  
Acid Sulfate Soil ◽  
Acid Sulfate
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