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

Yıl 2019, Cilt: 34 Sayı: 1, 93 - 101, 20.02.2019

Hasan Hadi Mahdi Mahdi Veli Uygur Burak Durgun

https://doi.org/10.7161/omuanajas.403794

Cited By: 1

Öz

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. 

Anahtar Kelimeler

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

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

Öz

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.

Anahtar Kelimeler

Atabey Ovası, Fosfor (P), Kemometrik Analizler, Sıralı Ekstraksiyon

Kaynakça

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