Soil geochemistry of the Bogotá River Basin

Authors

  • Gloria Prieto Instituto Colombiano de Geología y Minería
  • Luz Myriam González Instituto Colombiano de Geología y Minería
  • Orlando Vargas Instituto Colombiano de Geología y Minería
  • Adriana Matamoros Instituto Colombiano de Geología y Minería

DOI:

https://doi.org/10.32685/0120-1425/boletingeo.41.2006.156

Keywords:

soils, heavy metals, potentially dangerous elements, Bogotá, river basin, geochemistry

How to Cite

Prieto, G., González, L. M., Vargas, O., & Matamoros, A. (2006). Soil geochemistry of the Bogotá River Basin. Boletín Geológico, (41), 41–56. https://doi.org/10.32685/0120-1425/boletingeo.41.2006.156

Issue

Section

Articles

Published

2006-01-01

Abstract

In arder to study environmental geochemical processes in the Central Region of Colombia, the geochemistry project of Ingeominas, carried out a systematic geochemical sampling programme in soils a long the Bogotá River basin. The sampling program was carried out based on a bi-dimensional net (5x5km cells), collecting one sample per 25 km2 and one cell duplicate sample per 100 km2. 273 samples of superficial soil (A0-25) and Chorizan (up to 2m depth) were collected.

In the INGEOMINAS laboratories pseudototal contents of Cd, Pb, Zn, Mo, Mn, As, Cr, Co, Cu and Ni were determined (aqua regia and multi-acid digestion/ICP-AES); and in Activation Laboratories of Canada 48 elements were measured (multi-acid digestion/ICP-AES; INAA).

This paper presents results of As, Cd, Co, Cr, Cu, Mn, Mo, Ni, Pb, and Zn in the superficial horizon (A0-25) of the soil samples, including sorne data generated far previous projects carried out far INGEOMINAS in this region. The data were processed statistically and geo-statistically, dots and distribution maps by element were constructed.

Geochemical patterns allow differentiating two main zones. First zone covers the high basin of the Bogotá river including the Savannah of Bogotá, and the Capital City, the soils have acidic pH (pH 4-6,5), textura! variability and relatively low concentration of elements with the exception of sorne places in the middle basin. Second zone, comprises the low river basin, the soils have more basic pH (pH 6,6-9), texture predominantly argillaceous and high contents of trace elements.

Statistically three associátion groups were differentiated: group 1: As, Cd, Cu, Cr, Mo, Ni and Zn; group 2: Co and Mn and group 3: Pb, not displaying significant correlation with any other element. These groups correspond to natural geochemical associations characteristic of sedimentary rocks. They represent also common associations of residues of activities such us industry, agriculture and transport. Lead behaviour, on the other hand seems to indicate mainly anthropic origin (old leaded gasoline and industrial emissions).

The systematic soil sampling carried out along the Bogotá River basin, allowed to determine accumulation levels of potentially harmful elements, to discriminate possible origin and to analyze parameters and factors that determine local mobility and bio-availability of these elements. This information contributes to the geochemical base lines definition, is basic to soil use planning and is support to the Bogotá River basin management.

References

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