Rendgenska ispitivanja opekarsko-keramičkih glina iz ležišta "srednja strana"-Novi Bečej
X-ray investigations of the brick-ceramic clays from the ore deposit ''Srednja strana''–Novi Bečej
Abstract
With the X-ray method there were investigated numerous samples from the layers of the ceramic, brick and substratum clays, and also collective composites from the ore deposit “Srednja strana” – Novi Bečej, which were compared with the chemical and grain-size investigations. The results which were obtained with the X-ray and chemical investigations are in very good agreement, while the results which were obtained by grain-size method manifested something bigger disagreement.
All of the investigations indicate that mineral, chemical and grain-size compositions of the brick clays and collective composite samples are favorable than compositions of the ceramic clays.
It was established variation in the mineral composition by depth, and most characteristic is that carbonate content decrease from surface by depth, while content of the clay minerals and feldspars increase. In the ceramic and brick clay layers clay minerals are with two to three times more content than feldspars, while in t...he substratum clay layer they are of approximative contents.
Quartz is in all of the layers mineral with most content, and of clay minerals that are montmorillonite and illite. Vermiculite content decrease with depth. Kaolinite and chlorite is mostly with low content, and with something more content in the brick clay level.
Keywords:
Novi Bečej / ore deposit / X-ray investigations / mineral composition / quartz / clays / feldspars / carbonatesSource:
Radovi, 2004, 39, 221-236Publisher:
- Geoinstitut
Institution/Community
IHTMTY - JOUR AU - Tančić, Pavle AU - Janežić, Vesna PY - 2004 UR - https://cer.ihtm.bg.ac.rs/handle/123456789/6442 AB - With the X-ray method there were investigated numerous samples from the layers of the ceramic, brick and substratum clays, and also collective composites from the ore deposit “Srednja strana” – Novi Bečej, which were compared with the chemical and grain-size investigations. The results which were obtained with the X-ray and chemical investigations are in very good agreement, while the results which were obtained by grain-size method manifested something bigger disagreement. All of the investigations indicate that mineral, chemical and grain-size compositions of the brick clays and collective composite samples are favorable than compositions of the ceramic clays. It was established variation in the mineral composition by depth, and most characteristic is that carbonate content decrease from surface by depth, while content of the clay minerals and feldspars increase. In the ceramic and brick clay layers clay minerals are with two to three times more content than feldspars, while in the substratum clay layer they are of approximative contents. Quartz is in all of the layers mineral with most content, and of clay minerals that are montmorillonite and illite. Vermiculite content decrease with depth. Kaolinite and chlorite is mostly with low content, and with something more content in the brick clay level. PB - Geoinstitut T2 - Radovi T1 - Rendgenska ispitivanja opekarsko-keramičkih glina iz ležišta "srednja strana"-Novi Bečej T1 - X-ray investigations of the brick-ceramic clays from the ore deposit ''Srednja strana''–Novi Bečej VL - 39 SP - 221 EP - 236 UR - https://hdl.handle.net/21.15107/rcub_cer_6442 ER -
@article{ author = "Tančić, Pavle and Janežić, Vesna", year = "2004", abstract = "With the X-ray method there were investigated numerous samples from the layers of the ceramic, brick and substratum clays, and also collective composites from the ore deposit “Srednja strana” – Novi Bečej, which were compared with the chemical and grain-size investigations. The results which were obtained with the X-ray and chemical investigations are in very good agreement, while the results which were obtained by grain-size method manifested something bigger disagreement. All of the investigations indicate that mineral, chemical and grain-size compositions of the brick clays and collective composite samples are favorable than compositions of the ceramic clays. It was established variation in the mineral composition by depth, and most characteristic is that carbonate content decrease from surface by depth, while content of the clay minerals and feldspars increase. In the ceramic and brick clay layers clay minerals are with two to three times more content than feldspars, while in the substratum clay layer they are of approximative contents. Quartz is in all of the layers mineral with most content, and of clay minerals that are montmorillonite and illite. Vermiculite content decrease with depth. Kaolinite and chlorite is mostly with low content, and with something more content in the brick clay level.", publisher = "Geoinstitut", journal = "Radovi", title = "Rendgenska ispitivanja opekarsko-keramičkih glina iz ležišta "srednja strana"-Novi Bečej, X-ray investigations of the brick-ceramic clays from the ore deposit ''Srednja strana''–Novi Bečej", volume = "39", pages = "221-236", url = "https://hdl.handle.net/21.15107/rcub_cer_6442" }
Tančić, P.,& Janežić, V.. (2004). Rendgenska ispitivanja opekarsko-keramičkih glina iz ležišta "srednja strana"-Novi Bečej. in Radovi Geoinstitut., 39, 221-236. https://hdl.handle.net/21.15107/rcub_cer_6442
Tančić P, Janežić V. Rendgenska ispitivanja opekarsko-keramičkih glina iz ležišta "srednja strana"-Novi Bečej. in Radovi. 2004;39:221-236. https://hdl.handle.net/21.15107/rcub_cer_6442 .
Tančić, Pavle, Janežić, Vesna, "Rendgenska ispitivanja opekarsko-keramičkih glina iz ležišta "srednja strana"-Novi Bečej" in Radovi, 39 (2004):221-236, https://hdl.handle.net/21.15107/rcub_cer_6442 .