Abstract

Regolith is the term we give parent material that h as been weathered. The regolith consists of weather ed bedrock near the surface including the soil layer. In the Iranian soil layer we will find: decayed par ent materials, decaying plant material, decaying animal matter (manure) along with vegetation. Results of the present study show us that methods stimulating natu ral fertility in Iran includes composting-adds humu s layer, drip irrigation-balances illuviation and elu viation in arid regions, crop rotation/ intercroppi ng-reflects natural diversity and limits gleization, add lime-r educes gleization, non-cultivation techniques-reduc es hard pan (calcification) caused by compaction and reduce pesticide use-keeps decomposers alive in humus layer.

Highlights

  • Eluviation is the downward movement of particles which occurs as water percolates into the soil from the surface

  • Humification is the term used to explain the downward movement of plant and animal waste into the soil layer through precipitation

  • Illuviation is the upward movement of minerals from parent materials which occurs as plants extract water from the soil

Read more

Summary

INTRODUCTION

Eluviation is the downward movement of particles (decaying vegetation and animal waste) which occurs as water percolates into the soil from the surface. This is related to the amount of precipitation a region receives. Humification is the term used to explain the downward movement of plant and animal waste into the soil layer through precipitation. Illuviation is the upward movement of minerals from parent materials which occurs as plants extract water from the soil This is called evapotranspiration by geographers and is related to the region’s temperature.

Processes Creating Soil Infertility
Salinization
Calcification
Gleization
Podzolization
Other Elements Creating Soil Fertility and Infertility in Iran
CONCLUSION

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 call

Disclaimer: 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.