Abstract
Seasonal Changes of Macro- and Microelements Content in Soils of Green Tea Farming from Rize (Turkey)
Highlights
Soil is a natural organic structure, having both mineral and organic constituents, in addition to biological, physical, and chemical features
In 86.6% of the soil samples the value of pH was recorded between 4.50 and 6.00, which is considered ideal for tea growing
Soil reaction has been gradually acidic and the soil productivity began to be lost as a result of manufacturers, especially using ammonium sulphate fertilizer alone and overmuch
Summary
Soil is a natural organic structure, having both mineral and organic constituents, in addition to biological, physical, and chemical features. The soil properties cannot be a simple reflexion on the connected features of all soil components. Chemical elements in soil refer to as trace elements (TEs), because of their occurrence at concentrations less than 100 mg∙kg-1. Many of these elements are present at concentrations much lower than this value. Soil is a combination of solid (mineral and organic section), liquid, and gaseous phases. The chemical combination of soil, and its mineral structure and the expression of distribution are significant factors, influencing soil properties
Sign-in/Register to view highlights & summary Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
