ÖZET : Daphan ovosı toprakları kısmen iisı pliosen-pleıstosen yaşlı alüviyal birikintiler ve kısmen
bu materyal üzerine taşınıp gelmiş, daha ince bünyeli bazaltik materyallerden, çayır örtüsü altında oluşmuşlardır.
Oluşumlarında hakim toprak oluş süreci kalsifikasyon'dur.
Ova topraklarında 12 toprak serisi belirlenmiş olup, bunlardan Alaca, Ermecik ve Ispiryolu serileri calciustert alt grubuna; Çiğdemli ve Makastarla serileri vertic calciusloll alt grubuna; Daphan. Orıadüzün Yeniköy serileri vertic haplustoll alı grubuna; Hûncivarı ve Tazegül serileri pachic calciusloll ait grubuna,
Suiagındüzler serisi tipik calciusloll alı grubuna ve Paşayurdu serisi ise enlic haplustoll alt grubuna
sokulmuşlardır.
SUMMARY : The Daphan Plain Soils have formed under grass vegetation, on the materials partly
aluvial deposits yvhich belong lo upper pliosen age and partly finer texıured hasaltic material which
transported and deposited. Dominant soil formation process is calciftcalion.
12 soil series were determined in the plain soils. They were included in the suh groups as follows:
Alaca, Ermecik and Ispiryolu series in udic calciustert sub group; Çiğdemli and Makastarla series in vertic
calciusloll sub group: Daphan, Orıadüzün and Yeniköy series in vertic haplustoll sub group; Hancivarı Tazegül series in pachic calciusloll sub group; Sıdağındüzler series in tipic calciusloll sub group and Paşayurdu
series in entic haplustoll sub group
Primary Language | tr;en |
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Journal Section | Makaleler |
Authors | |
Publication Date | January 3, 2011 |
Published in Issue | Year 1996 Volume: 27 Issue: 1 |
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