Relative contributions of abiotic and biological factors in Fe(II) oxidation in mine drainage

被引:123
|
作者
Kirby, CS [1 ]
Thomas, HM
Southam, G
Donald, R
机构
[1] Bucknell Univ, Dept Geol, Lewisburg, PA 17837 USA
[2] No Arizona Univ, Dept Biol Sci, Flagstaff, AZ 86011 USA
关键词
D O I
10.1016/S0883-2927(98)00071-7
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The oxidation of Fe(II) is apparently the rate-limiting step in passive treatment of coal mine drainage. Little work has been done to determine the kinetics of oxidation in such field systems, and no models of passive treatment systems explicitly consider iron oxidation kinetics. A Stella II model using Fe(II)(init) concentration, pH, temperature, Thiobacillus ferrooxidans and O-2 concentration, flow rate, and pond volume is used to predict Fe(II) oxidation rates and concentrations in seventeen ponds under a wide range of conditions (pH 2.8 to 6.8 with Fe(II) concentrations of less than 240 mg L-1) from 6 passive treatment facilities. The oxidation rate is modeled based on the combination of published abiotic and bic,logical laboratory rate laws. Although many other variables have been observed to influence Fe(II) oxidation rates, the 7 variables above allow field systems to be modeled reasonably accurately for conditions in this study. Measured T. ferrooxidians concentrations were approximately 10(7) times lower than concentrations required in the model to accurately predict field Fe(II) concentrations. This result suggests that either 1) the most probable number enumeration method underestimated the bacterial concentrations, or 2) the biological rate law employed underestimated the influence of bacteria, ol both. Due to this discrepancy, bacterial concentrations used in the model for pH values of less than 5 are treated as fit parameters rather than empirically measured values. Predicted Fe(II) concentrations in ponds agree well with measured Fe(II) concentrations, and predicted oxidation rates also agree well with field-measured rates. From pH 2.8 to approximately pH 5, Fe(II) oxidation rates are negatively correlated with pH and catalyzed by T. ferrooxidans. From pH 5 to 6.4, Fe(II) oxidation appears to be primarily abiotic and is positively correlated with pH. Above pH 6.4, oxidation appears to be independent of pH. Above pH 5, treatment efficiency is affected most by changing design parameters in the following order: pH > temperature approximate to influent Fe(II) > pond volume approximate to O-2. Little to no increase in Fe(II) oxidation rate occurs due to pH increases above pH 6.4. Failure to consider Fe(II) oxidation rates in treatment system design may result in insufficient Fe removal. (C) 1999 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:511 / 530
页数:20
相关论文
共 50 条
  • [1] Relative contributions of abiotic and biological factors in Fe(II) oxidation in mine drainage (vol 14, pg 511, 1999)
    Kirby, CS
    Thomas, HM
    Southam, G
    Donald, R
    APPLIED GEOCHEMISTRY, 1999, 14 (08) : 1101 - 1101
  • [2] EFFECT OF SOME ABIOTIC FACTORS ON THE FE(II) OXIDATION ACTIVITY
    BANHEGYI, J
    CSERHATI, T
    KECSKES, M
    ACTA MICROBIOLOGICA ACADEMIAE SCIENTIARUM HUNGARICAE, 1980, 27 (03): : 258 - 258
  • [3] Effect of co-existent Al(III) in As-rich Acid Mine Drainage (AMD) on As removal during Fe(II) and As(III) abiotic oxidation process
    Yuan, Zidan
    Ma, Xu
    Wang, Shaofeng
    Yu, Le
    Zhang, Peiwen
    Lin, Jinru
    Jia, Yongfeng
    JOURNAL OF WATER PROCESS ENGINEERING, 2021, 44
  • [4] Flume simulations of Fe oxidation and deposition in abandoned mine drainage
    Peterson, William
    Herman, Ellen
    McGuire, Molly
    ABSTRACTS OF PAPERS OF THE AMERICAN CHEMICAL SOCIETY, 2018, 255
  • [5] Iron isotope fractionation during Fe(II) oxidation and precipitation of iron in acid mine drainage (Carnoule's Mine, France)
    Egal, M.
    Casiot, C.
    Elbaz-Poulichet, F.
    GEOCHIMICA ET COSMOCHIMICA ACTA, 2008, 72 (12) : A238 - A238
  • [6] Comparing the relative contributions of biotic and abiotic factors as mediators of species' distributions
    Gonzalez-Salazar, Constantino
    Stephens, Christopher R.
    Marquet, Pablo A.
    ECOLOGICAL MODELLING, 2013, 248 : 57 - 70
  • [7] The relative contributions of biological and abiotic processes to carbon dynamics in subarctic sea ice
    Dorte Haubjerg Søgaard
    David N. Thomas
    Søren Rysgaard
    Ronnie Nøhr Glud
    Louiza Norman
    Hermanni Kaartokallio
    Thomas Juul-Pedersen
    Nicolas-Xavier Geilfus
    Polar Biology, 2013, 36 : 1761 - 1777
  • [8] The relative contributions of biological and abiotic processes to carbon dynamics in subarctic sea ice
    Sogaard, Dorte Haubjerg
    Thomas, David N.
    Rysgaard, Soren
    Glud, Ronnie Nohr
    Norman, Louiza
    Kaartokallio, Hermanni
    Juul-Pedersen, Thomas
    Geilfus, Nicolas-Xavier
    POLAR BIOLOGY, 2013, 36 (12) : 1761 - 1777
  • [9] Fe(II) oxidation during acid mine drainage neutralization in a pilot-scale sequencing batch reactor
    Zvimba, J. N.
    Mathye, M.
    Vadapalli, V. R. K.
    Swanepoel, H.
    Bologo, L.
    WATER SCIENCE AND TECHNOLOGY, 2013, 68 (06) : 1406 - 1411
  • [10] Biological Mn(II) oxidation under organic substrate-limited conditions and its application in mine drainage remediation
    Miyata, Naoyuki
    Suganuma, Reina
    Sunouchi, Kimihito
    Okano, Kunihiro
    Fuchida, Shigeshi
    Watanabe, Miho
    Fujibayashi, Megumu
    Sato, Yuya
    Tokoro, Chiharu
    BIOCHEMICAL ENGINEERING JOURNAL, 2024, 203