Site Implementation Plan: La Cienega, Cointzio, Mexico

Table of Contents

1. Site Information
2. Summary
3. Location description
   1. Soils
   2. Geology
   3. Annual rainfall and seasonality
   4. Location of experimental fields
4. Stakeholder information
5. Land use
6. Conservation measures and experimental setup
7. Monitoring
8. Analysis

Soils

Acrisol are formed by the alteration of the basaltic-andesitic lava. Erosion eroded the organic horizon. Actually, soils have at least 80 cm deep, clayish (60 a 75% clay), presenting a Bw between 40-70 cm full of Fe and Mn deposits due to the presence of water table, Bt between 70-120 cm with prismatic structure without any deposits of Fe and Mn, C > 120 cm pH 5,5, MO 4%, Da 1,3, hydraulic conductivity very low (< 1cm/h).