Hasan Hadi Mahdi Mahdi, Veli Uygur, Burak Durgun

Kireçli ana materyal üzerinde oluşan topraklarda fosfor fraksiyonları ile bazı toprak özellikleri arasındaki ilişkiler

Fosfor (P), birçok fizyolojik ve biyokimyasal süreçte önemli bir element olduğu için bilinen tüm canlılar için mutlak gereklidir. Toprak oluşum süreçlerine ve arazi kullanımına bağlı olarak ortaya çıkFosfor (P), birçok fizyolojik ve biyokimyasal süreçte önemli bir element olduğu için bilinen tüm canlılar için mutlak gereklidir. Toprak oluşum süreçlerine ve arazi kullanımına bağlı olarak ortaya çıkan toprak özellikleri topraklarda fosforunun yarayışlılığı ve jeokimyasal fraksiyonlarında değişikliklere neden olmaktadır. Bu çalışmada Atabey Ovası’ndan toplam 71 adet yüzey toprak örneği (0-20 cm) alınmıştır. Topraklarda kademeli fosfor fraksiyonlaması yapılmıştır. Bu fraksiyonlar; sodyum bikarbonat [NaHCO3-P (organik Po, inorganik Pi ve total Pt)], sodyum hidroksit [NaOH-P (organik Po, inorganik Pi ve total Pt)], sitrat bikarbonat dithionit (CBD-P), hidroklorik asit ile ekstrakte edilebilen (Ca-P) ve bakiye (Res-P) fosfor şeklindedir. Fosfor fraksiyonlarının toprak özellikleri ile olan ilişkileri tanımlayıcı istatistik analizleri, Pearson korelasyon analizi ve kemometrik analizlerle ortaya konulmaya çalışmıştır. Ova topraklarında fraksiyonların ortalama dağılım sırası büyükten küçüğe doğru Ca-P (% 50.36) > Res-P (% 19.94) > CBD-P (% 12.17) > NaOH-Pt(% 6.94) > NaOH-Pi(% 6.24) > NaHCO3-Pt (% 1.82) > NaHCO3-Pi(% 1.57) > NaOH-Po (% 0.71) > NaHCO3-Po (% 0.25) şeklinde izlenmiştir. Bu fraksiyonların oransal dağılımının arazi kullanım şekline bağlı gübreleme miktarına göre değiştiği belirlenmiştir.

The relations between phosphorus fractions and some soil properties in soils forming on calcareous parent material

Phosphorus (P) is essential to all known life forms because it is a key element in many physiological and biochemical processes. Soil properties due to soil formation processes and land use have impacts on the availability of phosphorus in soils and on the change in geochemical fractions. Thus, total of 71 surface soil samples (0-20 cm) were taken from the Atabey Plain. The sequential extraction procedure was executed in the samples. The determined fractions were: sodium bicarbonate [NaHCO3-P (organic Po, inorganic Pi and Total Pt)], sodium hydroxide [NaOH-P (organic Po, inorganic Pi and Total Pt)], citrate bicarbonate dithionite (CBD-P), hydrochloric acid (Ca-P), and residual (Res-P) phosphorus. Relations of phosphorus fractions with soil properties were revealed by descriptive statistics, Pearson correlation analysis and chemometric analysis. The average distribution of fractions in the plain soils in descending order were: Ca-P (% 50.36) > Res-P (% 19.94) > CBD-P (% 12.17) > NaOH-Pi(% 6.24) > NaHCO3-Pi(% 1.57) > NaOH-Po (% 0.71) > NaHCO3-Po (% 0.25). It was determined that the fractal distribution of these fractions changed according to the land use pattern-dependent on fertilizer usage.

Keywords:

Atabey Plain Phosphorus (P), Chemometric Analyses, Sequential Extraction,

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