THE MINERALOGICAL COMPOSITION OF THRACE ZEOLITIC ROCKS AND THEIR POTENTIAL USE AS FEED ADDITIVES AND NUTRITION SUPPLEMENTS


Δημοσιευμένα: Ιουλ 28, 2016
Λέξεις-κλειδιά:
Ζεόλιθος τύπου-HEU ινώδεις ζεόλιθοι μορντενίτης ανάλκιμο
A. Filippidis
N. Kantiranis
A. Tsirambides
Περίληψη
Τριάντα δύο (32) θέσεις ζεολιθικών πετρωμάτων της Θράκης (29 της ΠΕ Έβρου και 3 της ΠΕ Ροδόπης) μελετήθηκαν ως προς την ορυκτολογική τους σύσταση με την μέθοδο της περιθλασιμετρίας ακτίνων Χ (XRD). Σύμφωνα με τον Kανονισμό της ΕΕ αριθ. 651/2013, κλινοπτιλόλιθος ιζηματογενούς προέλευσης (ζεολιθικοί τόφφοι) με ≥80% κ.β. κλινοπτιλόλιθο, ≤20% κ.β. αργιλικά ορυκτά, χωρίς ίνες και χαλαζία, μπορεί να χρησιμοποιηθεί ως πρόσθετη ύλη ζωοτροφών για όλα τα ζωικά είδη. Τα ζεολιθικά πετρώματα της Θράκης κατά μέσο όρο περιέχουν, 23 89% κ.β. ζεόλιθο τύπου- HEU (κλινοπτιλόλιθο-ευλανδίτη), 8-45% κ.β. μορντενίτη (δέκα θέσεις), 24% κ.β. ανάλκιμο (μία θέση), 1-11% κ.β. μαρμαρυγία, 1-11% κ.β. αργιλικά ορυκτά, 3-37% κ.β. χαλαζία, 2-29% κ.β. χριστοβαλίτη, 3-34% κ.β. αστρίους και 0-22% κ.β. άμορφα υλικά. Μόνο μία θέση περιέχει 89% κ.β. ζεόλιθο τύπου-HEU (κλινοπτιλόλιθο-ευλανδίτη), 2% κ.β. αργιλικά ορυκτά, είναι χωρίς ίνες, αλλά δυστυχώς περιέχει 3% κ.β. χαλαζία και 2% κ.β. χριστοβαλίτη. Λαμβάνοντας υπόψη την ορυκτολογική σύσταση, τα ζεολιθικά πετρώματα της Θράκης δεν πληρούν τις απαιτήσεις του Kανονισμού της ΕΕ αριθ. 651/2013, και γι’ αυτό δεν μπορούν να χρησιμοποιηθούν ως πρόσθετη ύλη ζωοτροφών για όλα τα ζωικά είδη και επομένως ως συμπληρώματα διατροφής, επειδή τα ζεολιθικά πετρώματα όλων των θέσεων, περιέχουν κατά μέσο όρο 3-37% κ.β. χαλαζία, 2-29% κ.β. χριστοβαλίτη, 8-45% κ.β. μορντενίτη (ινώδη ζεόλιθο) σε 10 θέσεις, 24-65% κ.β. ζεόλιθους (τύπου-HEU ± μορντενίτη ± ανάλκιμο) σε 28 θέσεις, 74% κ.β. ζεόλιθο τύπου- HEU σε 2 θέσεις και 77% κ.β. ζεόλιθο τύπου-HEU σε 1 θέση.
Λεπτομέρειες άρθρου
  • Ενότητα
  • Πετρολογία και Ορυκτολογία
Λήψεις
Τα δεδομένα λήψης δεν είναι ακόμη διαθέσιμα.
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