Evidence map›Paper›PMID 27610307›Full record

ArticleSpringerPlus2016

The radius of influence of a combined method of in situ air sparging and soil vapor extraction in the intertidal sediments of Gomso Bay on the west coast of South Korea.

Jun-Ho Lee, Han Jun Woo, Kap-Sik Jeong, Kap-Song Park

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Article in SpringerPlus, 2016. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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4 · The record

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5 · Who and what money

Authors and funding

4 authors.

Jun-Ho LeeKorean Seas Geosystem Research Center, Korea Institute of Ocean Science & Technology (KIOST), 787, Haean-ro, Sangnok-gu, Ansan-si, Gyeonggi-do 15627 Korea.
Han Jun WooKorean Seas Geosystem Research Center, Korea Institute of Ocean Science & Technology (KIOST), 787, Haean-ro, Sangnok-gu, Ansan-si, Gyeonggi-do 15627 Korea.
Kap-Sik JeongKorean Seas Geosystem Research Center, Korea Institute of Ocean Science & Technology (KIOST), 787, Haean-ro, Sangnok-gu, Ansan-si, Gyeonggi-do 15627 Korea.
Kap-Song ParkDepartment of Environmental Science and Engineering, Hankuk University of Foreign Studies (HUFS), 81, Oedae-ro, Mohyeon-myeon, Cheoin-gu, Yongin-si, Gyeonggi-do 17035 Korea.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

backgroundIn situ air sparging (IAS) was undertaken at sites in the tidal flats of Mandol and Hajeon, on the west coast of South Korea, to estimate variations in the radius of influence (ROI).

resultsThe Mandol core sample consisted of sand and muddy sand 1.6-3.4 [Formula: see text] (average 2.3 [Formula: see text]) and contained water (average 15.10 %). The Hajeon core sample consisted of muddy sand, sandy silt, and muddy sandy gravel 1.31-4.44 [Formula: see text] (average 3.11 [Formula: see text]) and contained water (average 19.77 %). These sites differ in their sedimentary and geochemical characteristics. At the Mandol site, no H2S or combustible gas was detected during a 48-h sampling period, except for some volatile organic compounds (0.1-2.0 ppm) at the monitoring well during the initial 30 min. At the soil vapor extraction wells, CO2 and O2 varied by 850 ppm (690-1540 ppm) and 0.5 % (20.4-20.9 %), respectively. At the Hajeon site, CO2 and O2 varied from 580 to 1250 ppm and 20.6 to 20.9 %, respectively, during the 48-h sampling period.

conclusionsAt the Mandol site, an oxygen concentration of 20.6 % was assumed as the effective concentration, and the ROI was estimated to be 128.0 cm. However, at the Hajeon site the ROI was estimated to be 85.7 cm. The smaller effective ROI at the Hajeon site was likely caused by the thin aquifer and thin screens of the sparing well. This estimated ROI show that the remediation effectiveness varies greatly as a heterogeneities and anisotropies in the porous sediments. Besides, injection pressure, flow rate, pulsing or continuous mode, and the range of intrinsic permeability for most important characteristic of sediment (soil) type impacted the ROI. Therefore, the IAS method is more effective at a pervasive air flow sediments such as Mandol, which consists of sand and muddy sand than at a channelized site such as Hajeon.

Indexed as

Effective oxygenIn situ air spargingRadius of influenceSoil vapor extractionTidal flat

Identifiers

PMID27610307
PMCPMC4993732

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Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.