N Sakarya
Biographic Data
| ID | 4983680 |
|---|---|
| NAME | N Sakarya |
| GIVEN NAMES | N |
| FAMILY NAME | Sakarya |
| SIGNATURE | SAKARYA N |
| AFFILIATIONS | Cukurova University |
| ORCID | 0000-0001-7215-068X |
| VERIFIED | Yes |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 14 |
| WORKS AS AUTHOR | 4 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1990 |
| LATEST PUBLICATION YEAR | 1998 |
| H-INDEX | 2 |
Mineralogy and micromorphology of İznik ceramics
The study of İznik ceramics of different periods revealed that temperatures of about 800–900°C were produced during firing. Glass fragments added to the body for strengthening resulted in the formation of fibrous minerals as clusters in the pores and protruding in the glaze together with Ca and P rich minerals in the raw materials used. The pore size distribution of the pores indicates a uniform temperature rise and fall during the production of …
Fibrous minerals in 16th‐century iznik ceramics
The presence of uniform orientation patterns of pseudowollastonite indicates a uniform and slow increase of temperature in the furnaces used in the production of the 16th‐century Iznik ceramics. Determination of pseudowollastonite in rounded pores (d = 20–40 μm) in the glaze probably indicates formation of vapor phases in pores. © 1993 John Wiley & Sons, Inc
Mineralogy and micromorphology of chalcolithic and early bronze age Ikiztepe ceramics
The mineralogy and micromorphology of ceramics from the Ikiztepe site (Chalcolithic and Early Bronze) have firing characteristics that indicate low temperature levels and oxidizing conditions. Stress phenomena indicated by cracks most probably indicate a process of shrinkage. Illuviated clay suggests the occurrence of humid periods with vigorous precipitation, pluvials during the Holocene. Provenance of clays used for production of ceramics is de…
Preliminary study of the microstructure and mineralogy of 12th and 13th century ceramics, Samsat, Southeastern Turkey
The mineralogy and microstructure of 12th and 13th century ceramics from Samsat, Turkey were examined with an X‐ray diffractometer and scanning electron microscope. There is a highly vitrified interlayer between the glaze and body in these sherds that probably accounts for the high durability of these ceramics. the lower vitrification and uniformity of the body in these ceramics suggests that leftover glaze was not mixed with paste during manufac…
Preliminary study of the microstructure and mineralogy of 12th and 13th century ceramics, Samsat, Southeastern Turkey
The mineralogy and microstructure of 12th and 13th century ceramics from Samsat, Turkey were examined with an X‐ray diffractometer and scanning electron microscope. There is a highly vitrified interlayer between the glaze and body in these sherds that probably accounts for the high durability of these ceramics. the lower vitrification and uniformity of the body in these ceramics suggests that leftover glaze was not mixed with paste during manufac…
Mineralogy and micromorphology of chalcolithic and early bronze age Ikiztepe ceramics
The mineralogy and micromorphology of ceramics from the Ikiztepe site (Chalcolithic and Early Bronze) have firing characteristics that indicate low temperature levels and oxidizing conditions. Stress phenomena indicated by cracks most probably indicate a process of shrinkage. Illuviated clay suggests the occurrence of humid periods with vigorous precipitation, pluvials during the Holocene. Provenance of clays used for production of ceramics is de…
Mineralogy and micromorphology of İznik ceramics
The study of İznik ceramics of different periods revealed that temperatures of about 800–900°C were produced during firing. Glass fragments added to the body for strengthening resulted in the formation of fibrous minerals as clusters in the pores and protruding in the glaze together with Ca and P rich minerals in the raw materials used. The pore size distribution of the pores indicates a uniform temperature rise and fall during the production of …
Fibrous minerals in 16th‐century iznik ceramics
The presence of uniform orientation patterns of pseudowollastonite indicates a uniform and slow increase of temperature in the furnaces used in the production of the 16th‐century Iznik ceramics. Determination of pseudowollastonite in rounded pores (d = 20–40 μm) in the glaze probably indicates formation of vapor phases in pores. © 1993 John Wiley & Sons, Inc
Preliminary study of the microstructure and mineralogy of 12th and 13th century ceramics, Samsat, Southeastern Turkey
The mineralogy and microstructure of 12th and 13th century ceramics from Samsat, Turkey were examined with an X‐ray diffractometer and scanning electron microscope. There is a highly vitrified interlayer between the glaze and body in these sherds that probably accounts for the high durability of these ceramics. the lower vitrification and uniformity of the body in these ceramics suggests that leftover glaze was not mixed with paste during manufac…
Mineralogy and micromorphology of chalcolithic and early bronze age Ikiztepe ceramics
The mineralogy and micromorphology of ceramics from the Ikiztepe site (Chalcolithic and Early Bronze) have firing characteristics that indicate low temperature levels and oxidizing conditions. Stress phenomena indicated by cracks most probably indicate a process of shrinkage. Illuviated clay suggests the occurrence of humid periods with vigorous precipitation, pluvials during the Holocene. Provenance of clays used for production of ceramics is de…
Fibrous minerals in 16th‐century iznik ceramics
The presence of uniform orientation patterns of pseudowollastonite indicates a uniform and slow increase of temperature in the furnaces used in the production of the 16th‐century Iznik ceramics. Determination of pseudowollastonite in rounded pores (d = 20–40 μm) in the glaze probably indicates formation of vapor phases in pores. © 1993 John Wiley & Sons, Inc
Mineralogy and micromorphology of İznik ceramics
The study of İznik ceramics of different periods revealed that temperatures of about 800–900°C were produced during firing. Glass fragments added to the body for strengthening resulted in the formation of fibrous minerals as clusters in the pores and protruding in the glaze together with Ca and P rich minerals in the raw materials used. The pore size distribution of the pores indicates a uniform temperature rise and fall during the production of …
Ceramic (4 works) · Materials Science (4 works) · Metallurgy (4 works) · Mineralogy (4 works) · Composite material (3 works) · Geology (3 works) · Glaze (3 works) · Chemistry (2 works) · Cultural Heritage Materials Analysis (2 works) · Microstructure (2 works)