KOP'ta (Konya Ovası Projeleri) arazi kullanımı
The Use of soil at the Konya Plain Projects
- Tez No: 87290
- Danışmanlar: YRD. DOÇ. DR. ADNAN PINAR
- Tez Türü: Yüksek Lisans
- Konular: Coğrafya, Geography
- Anahtar Kelimeler: Arazi kullanımı, Bitki örtüsü, Konya Ovası, Konya Ovası Projesi, Sulama, Verim, Ürün çeşitlendirme, İklim, Land use, Vegetation, Konya Plain, Konya Plain Project, Irrigation, Yield, Product diversification, Climate
- Yıl: 1999
- Dil: Türkçe
- Üniversite: Selçuk Üniversitesi
- Enstitü: Sosyal Bilimler Enstitüsü
- Ana Bilim Dalı: Ortaöğretim Sosyal Alanlar Eğitimi Ana Bilim Dalı
- Bilim Dalı: Coğrafya Öğretmenliği Bilim Dalı
- Sayfa Sayısı: Belirtilmemiş.
Özet
ABSTRACT The study site is located in the South-West of Middle Anatolia at 1000 abase sea- level. When the study side is examined geologically and morphologically, it can be seen that the site is affected by the Hersinien Orogenes and took its main form with Alp- Orogenes. The Konya Plain, the connection of which was broken completelly with seas in Pliosen, became an evoporif lake-basin. It was covered at the Plehistosen-period with a 25 metres deep lake which drew back in three phases. Kuaterner,, spreaded at the surroundings of lakes and at the bottoms of valleys covers a wide area. The base of these substances,formed completely out of alluvions, is covered with layers of schist, konglomera, clay, sand and pebble (Atalay,1987). Examined morphologically, in the project site there is allmost all kind of earh suface formations bu generally plains are in common. Considering the area, mountains and plateous are the most commons after plains. Considering the climate, it is seen thaat annual mean temperature is 1 1.2 °C (Turkey 13.6 °C> in July 22.6 °C (Turkey 24.6 °C) in January 0.2 °C (Turkey 2.5 °C). As it is seen there is a difference between the mean temperature of the project site and Turkey. The reason for this is copntinental climate and height. The project site is one of the places where minimum rain falls in Turkey. As it can be seen the dispersion of rain both according to months and different fields of the project in the study site, there are differences (İNAN, 1988). The amount of the surface-water is 4753 hm3/year, the underground -water 1048/year and in total 5801hm3/yeast at the project site. As for the amount of soil, waterable land is 1 956 748 ha, economically waterable 462 275 ha. In the project- site, beside alluvion soil many other types of other soils are also seen (DSİ, 1997). As it is seen, the Konya plain is rich for soil potential but poor for its' water potential. The biggest sources of water for the Konya Plain is the Çarşamba stream and the Beyşehir Lake. These sources are able to water a limited area. In order to water much lager areas, different plans and projects were made. The waters which will be brought from the XIupper region of Göksu basin will be collected im Afşin, Bağbaşi and Bozkir dams, from these dams because of the Blue Tunnel Project, the flowing of the water to Konya-Çumr a Plain has been thought. In addition to these, with small streams, rivers, marshes, snow and rain water, collected in different stores, only 462 275 ha. area will be watered. For this, the study of plans, projects and enterprises at different stages are continued and approximately 46 % of the project is finished. When the KOP (The Projects of the Konya Plains) is completed an important change will happen in the crop-designs, planting areas and in the productivity of these affecting stock-breeding, positively. Thus leading to the development of industry branches depending on agriculture, to new occupational opportunities and so to social and economical development for the people in that region and it will also make an important contributipn to the economy of this country. XII
Özet (Çeviri)
ABSTRACT The study site is located in the South-West of Middle Anatolia at 1000 abase sea- level. When the study side is examined geologically and morphologically, it can be seen that the site is affected by the Hersinien Orogenes and took its main form with Alp- Orogenes. The Konya Plain, the connection of which was broken completelly with seas in Pliosen, became an evoporif lake-basin. It was covered at the Plehistosen-period with a 25 metres deep lake which drew back in three phases. Kuaterner,, spreaded at the surroundings of lakes and at the bottoms of valleys covers a wide area. The base of these substances,formed completely out of alluvions, is covered with layers of schist, konglomera, clay, sand and pebble (Atalay,1987). Examined morphologically, in the project site there is allmost all kind of earh suface formations bu generally plains are in common. Considering the area, mountains and plateous are the most commons after plains. Considering the climate, it is seen thaat annual mean temperature is 1 1.2 °C (Turkey 13.6 °C> in July 22.6 °C (Turkey 24.6 °C) in January 0.2 °C (Turkey 2.5 °C). As it is seen there is a difference between the mean temperature of the project site and Turkey. The reason for this is copntinental climate and height. The project site is one of the places where minimum rain falls in Turkey. As it can be seen the dispersion of rain both according to months and different fields of the project in the study site, there are differences (İNAN, 1988). The amount of the surface-water is 4753 hm3/year, the underground -water 1048/year and in total 5801hm3/yeast at the project site. As for the amount of soil, waterable land is 1 956 748 ha, economically waterable 462 275 ha. In the project- site, beside alluvion soil many other types of other soils are also seen (DSİ, 1997). As it is seen, the Konya plain is rich for soil potential but poor for its' water potential. The biggest sources of water for the Konya Plain is the Çarşamba stream and the Beyşehir Lake. These sources are able to water a limited area. In order to water much lager areas, different plans and projects were made. The waters which will be brought from the XIupper region of Göksu basin will be collected im Afşin, Bağbaşi and Bozkir dams, from these dams because of the Blue Tunnel Project, the flowing of the water to Konya-Çumr a Plain has been thought. In addition to these, with small streams, rivers, marshes, snow and rain water, collected in different stores, only 462 275 ha. area will be watered. For this, the study of plans, projects and enterprises at different stages are continued and approximately 46 % of the project is finished. When the KOP (The Projects of the Konya Plains) is completed an important change will happen in the crop-designs, planting areas and in the productivity of these affecting stock-breeding, positively. Thus leading to the development of industry branches depending on agriculture, to new occupational opportunities and so to social and economical development for the people in that region and it will also make an important contributipn to the economy of this country. XII
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