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N. Jordanov

3 linked publication records

Author: N. Jordanovclear all
Showing 1-3 of 3 records
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SGEM International Multidisciplinary Scientific GeoConference EXPO Proceedings; 21st SGEM International Multidisciplinary Scientific GeoConference Proceedings 2021, Energy and Clean Technologies
Publication

SINTERED GLASS-CERAMICS, SELF-GLAZED MATERIALS AND FOAMS FROM METALLURGICAL SLAG

(STEF92 Technology, 2021-12-20, N. Jordanov, Alexander Karamanov)

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The materials used for the synthesis are modified waste raw materials in the form of slags (up to 70 % wt.) with addition of quartz sand and calcium fluoride. The initial batch is being melted at 1400 oC and then quenched in water. The resulting glass frit is milled bellow 75 microns, pressed into “green” samples being exposed in a next stage to thermal scanning at different temperatures with different heating rates, holding temperatures and times. In the framework of present investigation is presented analysis of...

Recycling2021
10th International Multidisciplinary Scientific GeoConference SGEM2010
Publication

MAGNETIC METHODS FOR DELINEATION OF HEAVY METAL POLLUTION IN BURGAS REGION

(SGEM Scientific GeoConference, 2010, N. Jordanova, D. Jordanova)

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Magnetic susceptibility mapping and rock magnetic characterization of topsoils from southeastern Bulgaria near the Black sea coast was carried out for delineation of the anthropogenic pollution. The presence of strongly magnetic parent material (volcanites, volcanoclastic sediments) and various soil types (Vertisols, Luvisols, Chromic Cambisols, Planosols, Fluvisols) were taken into account by using normalization of the field susceptibilities to the median susceptibility value, calculated separately for each soil ...

Applied and Environmental Geophysics2010
7th International Scientific Conference - SGEM2007
Publication

APPLICATION OF MAGNETIC METHODS FOR ESTIMATION OF THE DEGREE OF SOIL POLLUTION IN THE AREA OF VARNA – DEVNJA INDUSTRIAL ZONE

(SGEM Scientific GeoConference, 2007, D. Jordanova, N. Jordanova)

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Magnetism of soils is determined by the amount of strongly magnetic minerals, which may have different origin – inherent from the parent rocks (lithogenic); “in situ” formed during pedogenesis (pedogenic) and anthropogenic – from atmospheric deposition of particulates emitted from various industrial productions, which together with heavy metals contain also magnetic fraction. Due to the latter contribution, magnetic susceptibility of strongly polluted topsoils is significantly higher than the signal of non...

Oil and Gas Exploration2007
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