Open AccessSeasonal Variability in Vadose Zone Biodegradation at a Crude Oil Pipeline Rupture Site
Author(s) -
Sihota N.J.,
Trost J.J.,
Bekins B.A.,
Berg A.,
Delin G.N.,
Mason B.,
Warren E.,
Mayer K.U.
Publication year - 2016
Publication title -
vadose zone journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.036
H-Index - 81
ISSN - 1539-1663
DOI - 10.2136/vzj2015.09.0125
Subject(s) - vadose zone , seasonality , soil gas , soil water , environmental science , soil respiration , carbon cycle , respiration , hydrology (agriculture) , environmental chemistry , soil science , geology , chemistry , ecology , ecosystem , botany , geotechnical engineering , biology
Core Ideas Contaminant mass loss rates vary seasonally. Vadose zone temperatures in the source zone correlate with rates of contaminant respiration. Natural soil respiration and gas transport seasonality affect mass loss estimates. Understanding seasonal changes in natural attenuation processes is critical for evaluating source‐zone longevity and informing management decisions. The seasonal variations of natural attenuation were investigated through measurements of surficial CO 2 effluxes, shallow soil CO 2 radiocarbon contents, subsurface gas concentrations, soil temperature, and volumetric water contents during a 2‐yr period. Surficial CO 2 effluxes varied seasonally, with peak values of total soil respiration (TSR) occurring in the late spring and summer. Efflux and radiocarbon data indicated that the fractional contributions of natural soil respiration (NSR) and contaminant soil respiration (CSR) to TSR varied seasonally. The NSR dominated in the spring and summer, and CSR dominated in the fall and winter. Subsurface gas concentrations also varied seasonally, with peak values of CO 2 and CH 4 occurring in the fall and winter. Vadose zone temperatures and subsurface CO 2 concentrations revealed a correlation between contaminant respiration and temperature. A time lag of 5 to 7 mo between peak subsurface CO 2 concentrations and peak surface efflux is consistent with travel‐time estimates for subsurface gas migration. Periods of frozen soils coincided with depressed surface CO 2 effluxes and elevated CO 2 concentrations, pointing to the temporary presence of an ice layer that inhibited gas transport. Quantitative reactive transport simulations demonstrated aspects of the conceptual model developed from field measurements. Overall, results indicated that source‐zone natural attenuation (SZNA) rates and gas transport processes varied seasonally and that the average annual SZNA rate estimated from periodic surface efflux measurements is 60% lower than rates determined from measurements during the summer.