2011
DOI: 10.1007/s12665-011-1422-0
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Pyrite mine waste and water mapping using Hymap and Hyperion hyperspectral data

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Cited by 23 publications
(22 citation statements)
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“…The test site covers one of the gossanous ridges overlying a massive sulphide lens next to Riotinto River. Within the test site, different iron-bearing facies occur, such as the gossan itself, massive sulphide, altered shale and river sediments under the influence of acidic mine drainage (AMD) (Riaza et al [25]). The Iberian pyrite belt is hosted in a north -vergent fold and thrust belt of late Variscan age (Soriano and Casas [26], Donaire et al [27]) extending from east of Setubal/Portugal to north of Seville/Spain.…”
Section: Test Sitementioning
confidence: 99%
“…The test site covers one of the gossanous ridges overlying a massive sulphide lens next to Riotinto River. Within the test site, different iron-bearing facies occur, such as the gossan itself, massive sulphide, altered shale and river sediments under the influence of acidic mine drainage (AMD) (Riaza et al [25]). The Iberian pyrite belt is hosted in a north -vergent fold and thrust belt of late Variscan age (Soriano and Casas [26], Donaire et al [27]) extending from east of Setubal/Portugal to north of Seville/Spain.…”
Section: Test Sitementioning
confidence: 99%
“…The upper coarse grain surfaces tend to oxidize rapidly, whereas fine grained sands and mud near the water underlie crusts with hydrated sulfate, and lose water easily during the dry season [38]. Areas of wider crust development display high spatial mineralogical heterogeneity, related to minor topographical features, such as cracks, boulders, or ponds which can be only several centimeters wide (Figure 11(d)).…”
Section: The Spatial Heterogeneity Of Coatings On Mine Sites and Rivementioning
confidence: 99%
“…Numerous studies employ airborne imaging spectroscopy data [1][2][3] to map potential areas of acid mine drainage (AMD) generation, taking advantage of the abundance of specific secondary iron minerals that are stable in a specific pH range, indicating AMD generating conditions [1].…”
Section: Introductionmentioning
confidence: 99%
“…This produces acid and ferrous iron [1][2][3]. Secondary iron minerals that are generated during this process and that can be discriminated by spectroscopy are jarosite, ferrihydrite, goethite and copiapite, for example [1,2].…”
Section: Introductionmentioning
confidence: 99%
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