Modified soil respiration model (URESP) extended to sub-zero temperatures for biostimulated petroleum hydrocarbon-contaminated sub-Arctic soils

被引:0
|
作者
Kim, Jihun [1 ]
Chang, Wonjae [1 ]
机构
[1] Univ Saskatchewan, Dept Civil Geol & Environm Engn, 57 Campus Dr, Saskatoon, SK S7N 5A9, Canada
基金
加拿大自然科学与工程研究理事会; 加拿大创新基金会;
关键词
Soil respiration model; Unfrozen water content; Sub-zero temperatures; Contaminated cold-climate soils; Petroleum hydrocarbons; Bioremediation; UNFROZEN WATER-CONTENT; IN-SITU BIODEGRADATION; FROZEN SOIL; MICROBIAL RESPIRATION; ORGANIC-MATTER; BIOREMEDIATION; COLD; FIELD; DEPENDENCE; DEGRADATION;
D O I
10.1016/j.scitotenv.2019.02.067
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
It has been increasingly reported that aerobic soil respiration activity (CO2 production and O-2 consumption) is measurable in frozen cold-climate soils. This study modifies the Generalized Respiration (GRESP) model, a function of soil temperature (T) and unfrozen water content (M), to cover the frozen, partially frozen and unfrozen phases of successfully bioremediated, petroleum hydrocarbon-contaminated, sandy sub-Arctic soils. The Michaelis-Menten equation was modified to express the observable change in unfrozen water content near 0 degrees C, which is related to soil respiration activity during soil phase changes and at temperatures below the effective endpoint of detectable unfrozen water at -2 degrees C. The modified Michaelis-Menten equation was further combined with a Q(10) temperature term, and was then incorporated into the GRESP equation to produce a new URESP model for the engineered soil bioremediation system at sub-zero temperatures. The URESP model was applied to published input data measured from the biostimulated site soils of a pilot-scale soil tank experiment conducted between -5 and 15 degrees C.The model fit well with the experimental data for CO2 production (R-2 = 0.96) and O-2 consumption (R-2 = 0.92). A numerical soil thermal model (TEMP,AN model) of the thawing biotreated soils in the tank was also used in this study to produce valid alternative (predictive) input T and M data for the URESP model. The URESP-derived respiration quotients (RQ; 0.695 to 0.698), or the ratios of CO2 production to O-2 consumption, aligned with the experimental RQ values from the soil tank experiment (0.69) and fell within the theoretical RQ range for aerobic hydrocarbon degradation (0.63-0.80). The URESP model combined with the TEMP/ W simulation approximated changes in soil respiration during thawing and characterized the computed soil respiration outputs as related to hydrocarbon utilization, based on their RQ values. (C) 2019 Elsevier B.V. All rights reserved.
引用
收藏
页码:400 / 411
页数:12
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