Entisol ordosuna ait bir arazide bazı toprak özelliklerinin değişiminin belirlenmesi

Topraklar, doğal süreçler ve amenajman uygulamalarının farklı mekansal ve zamansal ölçeklerde etkilerinin sonucu değişkenliğe sahiptirler. Bu çalışmanın amacı daha önce detaylı temel toprak haritası hazırlanmış Entisol ordosuna ait bir arazide bazı toprak özelliklerinin değişimini ve haritalama üniteleri arasındaki farklılıkları ortaya koymaktır. Bu amaçla dört farklı haritalama ünitesini içine alan 400x800 m boyutlarında bir alandan örnekleme yapılmıştır. Toplam 512 toprak örneği 25x25m grid örnekleme düzeniyle 0-30 cm derinlikten alınmıştır. Varyasyon katsayısı değerlerine göre en yüksek değişkenlik gösteren toprak özelliği organik madde, en düşük ise toprak pH’sidir. Tüm alanda normal dağılım gösteren tek toprak özelliği değişebilir K’dır. Çalışma alanı haritalama ünitelerine bölündüğünde normal dağılım gösteren toprak özelliği sayısı artmıştır. ANOVA ve LSD test sonuçlarına göre, kil içeriği bakımından tüm harita üniteleri birbirinden farklıdır. Gerçek ortalamanın %10’u hata seviyesinde en çok 54 ile organik madde, en az ise 1 örnek ile toprak pH ‘sı için gereklidir. Tüm özellikler birlikte değerlendirildiğinde çalışma alanını temsil için 25 örnek gereklidir.

Determination of the variability of some soil properties on an field classified as Entisol

Soils have variations resulting from natural processes and management practices affected in different spatial and tem- poral scales. The aims of this study are to introduce the variability of some soil properties and exhibit the differences of soil mapping units (classified as Entisol) in an area having a detailed soil survey report. Soil samples were collected within an area of 400x800 m including four different soil mapping units. Soil samples, total of 512, were collected with a 25x25 m grid sampling design from 0-30 cm depth. Organic matter was the most variable and soil pH was the least variable soil properties based on coefficient of variation values. Exchangeable K was the only property exhibited normal distribution within whole study area. The number of soil properties with normal distribution was increased when the study area was divided into soil mapping units. The results of ANOVA and LSD test, showed that soil mapping units were significantly different from each other in clay content. In the study area 54 soil samples were required for organic matter and 1 soil sample was for soil pH to estimate average values in 10% error within true mean. All soil properties studied were considered together, 25 soil samples were required to represent the whole study area.

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