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COMUNICAÇÃO TÉCNICA ______________________________________________________________________________________________________________________________________________________________________________________________________
Nº 174753
High resolution techniques for geoenvironmental characterization of a site with methane in the subsoil Leandro Gomes de Freitas Marco Aurélio Zequim Pede Chang Hung Kiang
Trabalho apresentado no INTERNATIONAL CONTAMINATED SITE REMEDIATION CONFERENCE, CLEAN UP, 7th., 2017,
Melbourne. Proceedings...
A série “Comunicação Técnica” compreende trabalhos elaborados por técnicos do IPT, apresentados em eventos, publicados em revistas especializadas ou quando seu conteúdo apresentar relevância pública. ___________________________________________________________________________________________________
Instituto de Pesquisas Tecnológicas do Estado de São Paulo S/A - IPT
Av. Prof. Almeida Prado, 532 | Cidade Universitária ou Caixa Postal 0141 | CEP 01064-970
São Paulo | SP | Brasil | CEP 05508-901 Tel 11 3767 4374/4000 | Fax 11 3767-4099
www.ipt.br
HIGH RESOLUTION TECHNIQUES FOR GEOENVIRONMENTAL CHARACTERIZATION OF A SITE
WITH METHANE IN THE SUBSOIL
Leandro Gomes de Freitas1, Marco Aurélio Z. Pede2, Chang Hung Kiang2
1Geoenvironmental Technologies Center - CTGeo, Institute for Technological Research – IPT,São Paulo, BRAZIL
2Laboratory of Watershed Studies - LEBAC, Institute of Geosciences and Exact Sciences, São Paulo State University – UNESP, Rio Claro, BRAZIL
Introduction
Contaminated sites: risks associated with gas and vapour intrusionsin buildings.
Source: adapted from ITRC (2009).
CH4 contaminated sites: social, political and economic concerns
Center Norte Shopping Mall Cingapura Housing USP Leste University
Source: G1.globo.com (10/10/11)Source: G1.globo.com (28/09/11) Source: Folhapress (17/11/11)
How to obtain better site diagnostics?
High Resolution Site Characterization (HRSC)
Source: USEPA (2011)
Objective
Evaluate the application of the MIP with otherauxiliary techniques for site characterization withmethane occurrence in the subsoil.
Methodology
Three stages, including laboratory and fieldprocedures;
• 1st Stage: Bench testsFoto 9: Preparação das misturas gasosa. Foto 10: Injeção das misturas gasosas
na sonda MIP.
Preparation and injection of the gaseous mixtures in the MIP system
2nd Stage: Field tests
Tests with the Soil
Color Optical
Screening Tool
(SCOST)
Direct push (whole
core) soil sampling
2nd Stage: Field tests
Soil Gas sampling with Post Run Tubing System (PRT)
Foto 6: Ensaio de amostragem direta de gases do solo pelo sistema PRT.
3rd Stage: Laboratory analysis of soil samples
Grain size, organic matter and fraction of organic carbon analysis
Foto 23: Abertura dos liners em bancada de laboratório.
Foto 24: Descrição táctil visual e coleta de amostras de solo para caracterização
geotécnica.
Soil description and sample collection
MIP Field results - electric conductivity sensor (EC)
De
pth
(m)
EC/P1(mS/m)
EC/P2(mS/m)
EC/P3(mS/m)
EC/P4(mS/m)
EC/P5(mS/m)
EC/P6(mS/m)
0
1
2
3
4
5
6
7
8
9
10
11
A A’180 m
Geo-electrical cross section of study area (São Paulo Basin)
De
pth
(m)
EC/P1(mS/m)
EC/P2(mS/m)
EC/P3(mS/m)
EC/P4(mS/m)
EC/P5(mS/m)
EC/P6(mS/m)
A A’180 m
“ T E R T I A R Y ” ( S T r )
“ C O A R S E ” ( S Q a – F A r e )
“ T R A N S I T I O N ” ( S Q a - T r a n s )
“ F I N E ” ( S q a – A r g )
“ I N T E R B E D D E D ” ( D T e c )
“ F I N E ” ( D T e c )
“ C O A R S E ” O R “ F I N E ” ( D T e c )
????
?
?
0
1
2
3
4
5
6
7
8
9
10
11
De
pth
(m)
Groundwaterlevel
LithostratigraphicCharacterization
Lithostratigraphy
Technogenic Deposits
QuaternarySediments -
Silty Clay Lithofacies
QuaternarySediments -Transition
QuaternarySediments -
Sandy Lithofacies
Tertiary Sediments
Conclusion
• MIP/EC can provide high resolution response for:• Soil electrical conductivity - Lithostratigraphy;• Detection and mapping of METHANE in the subsurface
(FID);
• Auxiliary field and laboratory techniques also providedvaluable information to support the interpretation andvalidation of the results;
• HRSC techniques contributed to achieve a detailed CSMfor the presence of methane in the study area.
Thank you
Leandro Gomes de Freitas
Institute for Technological Research - IPT