Iron and manganese status in Sidi Barrani soils as a criterion for soil genesis and formation [electronic resource].

By: Contributor(s): Language: English Summary language: Arabic Description: p.71-94Other title:
  • صور الحديد والمنجنيز كدالة لاصل وتكوين أراضى سيدى براني"الساحل الشمالي الغربي".‪‪‪‪‪ [Added title page title]
Uniform titles:
  • Zagazig journal of agricultural research, 2008 v. 35 (1) [electronic resource].
Subject(s): Online resources: In: Zagazig Journal of agricultural research 2008.v.35(1)Summary: The current study is performed on 20 soil profiles representing the two major geomorphic units recognized in Sidi Barani area mainly: the coastal plain and the piedmont plain to evaluate Fe and Mn status and distribution and their relation to soil variables initiated by soil origin and pedogenetic processes ifvolved in soil formation. The obtained results clearly show that total Fe ranged from 2400 to 7020 ppm and 2500 to 7700 ppm in the soils of the coastal and piedmont plains, respectively. Total :Mn varies widely from 140 to 300 ppm and from 140 to 342 ppm in those plains, respectively.
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The current study is performed on 20 soil profiles representing the two major geomorphic units recognized in Sidi Barani area mainly: the coastal plain and the piedmont plain to evaluate Fe and Mn status and distribution and their relation to soil variables initiated by soil origin and pedogenetic processes ifvolved in soil formation. The obtained results clearly show that total Fe ranged from 2400 to 7020 ppm and 2500 to 7700 ppm in the soils of the coastal and piedmont plains, respectively. Total :Mn varies widely from 140 to 300 ppm and from 140 to 342 ppm in those plains, respectively.

Summary in Arabic.

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