Issue: March 29, 2008
How does our soil lock-up minerals?
I keep hearing that our soil is very alkaline, that it has a high pH, and that this "locks up the minerals in the soil" and keeps them unavailable to our plants. This situation happens in all deserts.
Can you explain how desert soil becomes alkaline, how the pH is affected by desert conditions, what "minerals locked up in our soil" means, and how a more neutral pH can make minerals and other nutrients more available to our plants? This is such a mystery to me!
This is a topic that cannot be thoroughly covered in the space allotted to a newspaper column, but it is a very good questions and important to understanding gardening in the Southwestern U.S. and other arid regions. I will answer it to at least initiate your understanding, but for a more through understanding I would recommend that you look for a course in soil science at a university or community college.
The first part of the answer requires a discussion of soil formation. Soils form as the rocks in the region (called parent material) are broken down and "weathered" to form soil. This is a complex process involving physics, chemistry, and biology. Rocks are broken into smaller pieces by gravity, freezing and thawing, and the effects of water. Some of the minerals in the rocks are then further modified by the water which dissolves the readily soluble components and carries these minerals away. This "weathering" of rock is enhanced by biological activity.
For more gardening information, visit the NMSU Extension publications World Wide Web site at http://www.cahe.nmsu.edu/pubs/_h.
Send your gardening questions to:
Yard and Garden, ATTN: Dr. Curtis Smith
NMSU Cooperative Extension Service
9301 Indian School Road, NE, Suite 112
Albuquerque, NM 87112
Curtis W. Smith, Ph.D., is an Extension Horticulture Specialist with New Mexico State University's Cooperative Extension Service. New Mexico State University is an equal opportunity/affirmative action employer and educator.