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Amaç: Çalışmada Gaziantep ili Nizip ilçesi zeytin bahçeleri topraklarının bor durumunun belirlenmesi amaçlanmıştır. Yöntem ve Bulgular: Bu amaç için Gaziantep ili Nizip ilçesi zeytin bahçeleri topraklarının temsil edecek şekilde iki farklı derinlikten (0-30 ve 30-60 cm) ve 20 farklı noktadan olmak üzere toplamda 40 toprak örneği alınmıştır. Örneklerde toprakların tekstür, pH, tuz, kireç ve yarayışlı bor içerikleri belirlenmiştir. Genel Yorum: Araştırma sonuçlarına gore; toprakların pH içerikleri 7.93-8.44; tuz içerikleri % 0.010-0.043; kil içerikleri % 33.04-61.04; kum içerikleri % 11.68-35.36; silt içerikleri % 18.32-50.32; kireç içerikleri % 8.11-93.28 ve alınabilir bor içerikleri 0.06-1.18 ppm arasında bulunmuştur. Bahçe topraklarının bor içeriği bakımından, 0-30 cm derinlikte % 85.00’inin çok az, % 10.00’u az ve % 5.00’nin yeterli düzeyde, 30-60 cm derinlikte ise % 95.00’i çok az ve % 5.00’i az düzeyde olduğu belirlenmiştir. Çalışmanın Önemi ve Etkisi: Çalışmada toprakların alınabilir bor içerikleri ile sadece silt içeriği arasında negatif önemli bir ilişki belirlenmiştir. Diğer yandan, toprakların tuz içeriği ile kum ve kireç içerikleri arasında negatif, kil içerikleri arasında ise pozitif önemli ilişkiler belirlenmiştir. Ayrıca, toprakların kil içerikleri ile kum, silt ve kireç içerikleri arasında negatif ve silt içeriği ile kireç içeriği arasında ise pozitif önemli ilişkiler belirlenmiştir.
Purpose: In the study, Gaziantep or Nizip district olive gardens are aimed at determining the bor state of the land. Method and findings: For this purpose, a total of 40 land samples from two different depths (0-30 and 30-60 cm) and 20 different points have been taken to represent the soil of the Olive Gardens of the province of Gaziantep and Nizip. In examples, the texture, pH, salt, grapefruit and beneficial bor content of the soil are determined. Overview: above the research results; the pH content of the soil was 7.93-8.44; the salt content was 0.010-0.043; the dust content was 33.04-61.04; the sand content was 11.68-35.36; the dust content was 18.32-50.32; the dust content was 8.11-93.28 and the bor content was 0.06-1.18 ppm. In terms of the bor content of the garden soil, at 0-30 cm depths 85. 00 is very little, 10.00 is less, and 5.00 is sufficient, and at a depth of 30-60 cm 95.00 is very little, and 5.00 is very low. The importance and impact of the study: The study has determined a negative significant relationship between the absorbable bor content of the soil and only the silk content. On the other hand, there have been positive significant relationships between the salt content of the soil and the content of sand and peanut but between the content of peanut. Moreover, positive important relationships have been established between the content of the soil and the content of the sand, silk and silk, and between the content of silk and silk.
Aims: The aim of this study was to determine the boron status of olive orchard in Nizip district of Gaziantep. Methods and Results: For this purpose, a total of 40 soil samples were taken from two different depths (0-30 and 30-60 cm) and 20 different points to represent the olive gardens. Texture, pH, salt, lime and useful boron contents of the soil were determined in the samples. Conclusions: According to the results of the research; pH contents of soils 7.93-8.44; salt contents of 0.010-0.043%; clay contents 33.04-61.04%; sand contents 11.68-35.36%; silt contents of 18.32-50.32%; lime contents were found between 8.11-93.28% and the contents of boron were found to be between 0.06-1.18 ppm. In terms of boron content of garden soils, at 0-30 cm depth, 85.00% is very small, 10.00% is less and 5.00% is sufficient, at 30-60 cm depth 95.00% is very small and 5.00% is low It is determined to be. Significance and Impact of the Study: In the study, it was determined that there is a negative significant relationship between the available boron content and silt content of soil. On the other hand, it was determined that while there is a negative significant relationship between salt content and sand and lime contents, there is a positive one between salt content and clay content of the soil. In addition, it was determined that whereas there is a negative significant relationship between clay content and sand, silt and lime contents, there is a positive significant relationship between silt content and lime content of the soil.
Alan : Ziraat, Orman ve Su Ürünleri
Dergi Türü : Ulusal
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