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PERSPECTIVE OF EXPLOITATION OF ALGINIT IN PLANT NUTRITION
J. KULICH
J. VALKO
D. OBERNAUER
Sažetak
Ore and non-ore potential of the Slovak Republic is restricted by the size of its area. Each successful result of
geological research uncovering modest raw material supplies is considered to be worthy. Since 1990 the
alginite bed situated in Lučenec Valley, locality of Picniná village, has been considered in the above
mentioned sense. Alginite represents a rock with relatively high organic matter content which was sedimenting
together with the clays in post - volcanic outbursts during geological periods appropriate for algae occurrence.
An interest for this material is also stimulated by the experiences obtained during alginite mining from the
deposit not far off Slovak - Hungarian boundary in Gercei and Pula in Hungary. Gercei alginite has a wide
variety of utilization as an ecological raw material. By underlining pedological and agrochemical alginite
value we intend to contribute to the realization of its utilization, especially in agriculture. First of all, the fact
that specific and volume weight as well as the consistent constants and particularly specific surface value of
alginite exclusively positively influence physical and chemical soil properties should be emphasized here.
Content of biogenic and trace elements, portion of colloidal fraction, humus content and sorption capacity
have a determinative significance for prospective alginite involving into an assortment of progressive
preparations for soil properties improving. Natural character, absence of phytotoxicity, effective economy of
mining technology and ecologization of farming systems, those are the arguments for alginite to be included
among such materials like zeolites and bentonites which have already achieved a possition for useful
agricultural utilization.
Ključne riječi
alginite; mineralogical composition; physical and chemical characteristics; utilization; soil properties; plant nutrition
Hrčak ID:
16018
URI
Datum izdavanja:
21.3.2002.
Posjeta: 2.382 *