Elibrary Perpustakaan Universitas Riau

Ebook, artikel jurnal dan artikel ilmiah

  • Beranda
  • Informasi
  • Berita
  • Bantuan
  • Pustakawan
  • Area Anggota
  • Pilih Bahasa :
    Bahasa Arab Bahasa Bengal Bahasa Brazil Portugis Bahasa Inggris Bahasa Spanyol Bahasa Jerman Bahasa Indonesia Bahasa Jepang Bahasa Melayu Bahasa Persia Bahasa Rusia Bahasa Thailand Bahasa Turki Bahasa Urdu

Pencarian berdasarkan :

SEMUA Pengarang Subjek ISBN/ISSN Pencarian Spesifik

Pencarian terakhir:

{{tmpObj[k].text}}
No image available for this title
Penanda Bagikan

e-journal

Geochemical processes controlling fate and transport of arsenic in acid mine drainage (AMD) and natural systems

Hefa Cheng - Nama Orang; Yuanan Hu - Nama Orang; Jian Luo - Nama Orang; Bin Xu - Nama Orang; Jianfu Zhao - Nama Orang;

Abstract.
Acid mine drainage (AMD) is often accompanied with elevated concentrations of arsenic, in the forms
of arsenite, As(III), and/or arsenate, As(V), due to the high affinity of arsenic for sulfide mineral ores.
This review summarizes the major geochemical processes controlling the release, speciation, fate, and
distribution of inorganic arsenic in mine drainage and natural systems. Arsenic speciation depends highly
on redox potential and pH of the solution, and arsenite can be oxidized to the less toxic arsenate form.
Homogeneous oxidation of arsenite occurs rather slowly while its heterogeneous oxidation on mineral
surfaces can greatly enhance the reaction rates. Little evidence suggests that precipitation reaction limits
the concentrations of arsenic in natural water, while co-precipitation may lead to rapid arsenic removal
when large amount of iron hydroxides precipitate out of the aqueous phase upon neutralization of the
mine drainage. Both arsenate and arsenite adsorb on common metal oxides and clay minerals through
formation of inner-sphere and/or outer-sphere complexes, controlling arsenic concentration in natural
water bodies. Arsenite adsorbs less strongly than arsenate in the typical pH range of natural water and is
more mobile. Part of the adsorbed arsenic species can be exchanged by common anions (e.g., PO43− and SO42−), especially phosphate, which leads to their re-mobilization. Understanding the geochemistry of arsenic is helpful for predicting its mobility and fate inAMDand natural systems, and for designing of costeffective
remediation/treatment strategies to reduce the occurrence and risk of arsenic contamination.

Keywords:
Arsenate
Arsenite
Fate and transport
Acid mine drainage (AMD)
Sorption


Ketersediaan

Tidak ada salinan data

Informasi Detail
Judul Seri
Journal of Hazardous Materials
No. Panggil
-
Penerbit
London : Elsevier B.V.., 2009
Deskripsi Fisik
Journal of Hazardous Materials 165 (2009) 13–26
Bahasa
English
ISBN/ISSN
-
Klasifikasi
-
Tipe Isi
-
Tipe Media
-
Tipe Pembawa
-
Edisi
-
Subjek
LINGKUNGAN HIDUP
Info Detail Spesifik
-
Pernyataan Tanggungjawab
agus
Versi lain/terkait

Tidak tersedia versi lain

Lampiran Berkas
  • Geochemical processes controlling fate and transport of arsenic in acid mine drainage (AMD) and natural systems
Komentar

Anda harus masuk sebelum memberikan komentar

Elibrary Perpustakaan Universitas Riau
  • Informasi
  • Layanan
  • Pustakawan
  • Area Anggota

Tentang Kami

As a complete Library Management System, SLiMS (Senayan Library Management System) has many features that will help libraries and librarians to do their job easily and quickly. Follow this link to show some features provided by SLiMS.

Cari

masukkan satu atau lebih kata kunci dari judul, pengarang, atau subjek

Donasi untuk SLiMS Kontribusi untuk SLiMS?

© 2025 — Senayan Developer Community

Ditenagai oleh SLiMS
Pilih subjek yang menarik bagi Anda
  • Karya Umum
  • Filsafat
  • Agama
  • Ilmu-ilmu Sosial
  • Bahasa
  • Ilmu-ilmu Murni
  • Ilmu-ilmu Terapan
  • Kesenian, Hiburan, dan Olahraga
  • Kesusastraan
  • Geografi dan Sejarah
Icons made by Freepik from www.flaticon.com
Pencarian Spesifik
Kemana ingin Anda bagikan?