Unsaturated seepage analysis at the Guayabo National Archaeological Monument, Costa Rica

The Guayabo National Archaeological Monument is considered one of the most important historical and political ceremonial centers of pre-Columbian Costa Rica, Central America, and it depicts the ingenuity and the quality of life of Costa Rica´s inhabitants between 800 BC and AD 1400. This site was na...

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Main Author: Baltodano-Goulding Rafael
Format: Article
Language:English
Published: EDP Sciences 2020-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/55/e3sconf_e-unsat2020_01026.pdf
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spelling doaj-6fc54913a61e4c0ea91b9ec83c4b215a2021-04-02T17:16:13ZengEDP SciencesE3S Web of Conferences2267-12422020-01-011950102610.1051/e3sconf/202019501026e3sconf_e-unsat2020_01026Unsaturated seepage analysis at the Guayabo National Archaeological Monument, Costa RicaBaltodano-Goulding RafaelThe Guayabo National Archaeological Monument is considered one of the most important historical and political ceremonial centers of pre-Columbian Costa Rica, Central America, and it depicts the ingenuity and the quality of life of Costa Rica´s inhabitants between 800 BC and AD 1400. This site was named International Historic Civil Engineering Landmark in 2009 by the American Society of Civil Engineers (ASCE). Evaluation of the unsaturated flow at the Northwestern slope using a two-dimensional model was performed. It was determined from field and modeling that at a relatively shallow depth the soil is relatively impermeable; thus, producing a large amount of run-off that tends to deteriorate the archaeological structures, and induce landslides. As part of the site investigation, exploratory borings were performed, and piezometers were installed in the upper, middle, and bottom parts of the slope. A series of laboratory testing was also performed to obtain index soil and permeability properties. The soil-water characteristic used to develop the K-Curve was also obtained. Additionally, a groundwater model was created using the geotechnical model and a water balance analysis for the area, where different scenarios of recharge and precipitation were analyzed taking into consideration the observed data. The volume of slope run-off through towards the archaeological site was estimated and the areas where it emerges, as well as the field groundwater.https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/55/e3sconf_e-unsat2020_01026.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Baltodano-Goulding Rafael
spellingShingle Baltodano-Goulding Rafael
Unsaturated seepage analysis at the Guayabo National Archaeological Monument, Costa Rica
E3S Web of Conferences
author_facet Baltodano-Goulding Rafael
author_sort Baltodano-Goulding Rafael
title Unsaturated seepage analysis at the Guayabo National Archaeological Monument, Costa Rica
title_short Unsaturated seepage analysis at the Guayabo National Archaeological Monument, Costa Rica
title_full Unsaturated seepage analysis at the Guayabo National Archaeological Monument, Costa Rica
title_fullStr Unsaturated seepage analysis at the Guayabo National Archaeological Monument, Costa Rica
title_full_unstemmed Unsaturated seepage analysis at the Guayabo National Archaeological Monument, Costa Rica
title_sort unsaturated seepage analysis at the guayabo national archaeological monument, costa rica
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2020-01-01
description The Guayabo National Archaeological Monument is considered one of the most important historical and political ceremonial centers of pre-Columbian Costa Rica, Central America, and it depicts the ingenuity and the quality of life of Costa Rica´s inhabitants between 800 BC and AD 1400. This site was named International Historic Civil Engineering Landmark in 2009 by the American Society of Civil Engineers (ASCE). Evaluation of the unsaturated flow at the Northwestern slope using a two-dimensional model was performed. It was determined from field and modeling that at a relatively shallow depth the soil is relatively impermeable; thus, producing a large amount of run-off that tends to deteriorate the archaeological structures, and induce landslides. As part of the site investigation, exploratory borings were performed, and piezometers were installed in the upper, middle, and bottom parts of the slope. A series of laboratory testing was also performed to obtain index soil and permeability properties. The soil-water characteristic used to develop the K-Curve was also obtained. Additionally, a groundwater model was created using the geotechnical model and a water balance analysis for the area, where different scenarios of recharge and precipitation were analyzed taking into consideration the observed data. The volume of slope run-off through towards the archaeological site was estimated and the areas where it emerges, as well as the field groundwater.
url https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/55/e3sconf_e-unsat2020_01026.pdf
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