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Frontiers of Earth Science

ISSN 2095-0195

ISSN 2095-0209(Online)

CN 11-5982/P

邮发代号 80-963

2019 Impact Factor: 1.62

Frontiers of Earth Science  0, Vol. Issue (): 395-405   https://doi.org/10.1007/s11707-013-0404-9
  RESEARCH ARTICLE 本期目录
Soil concentrations and soil-air exchange of organochlorine pesticides along the Aba profile, east of the Tibetan Plateau, western China
Soil concentrations and soil-air exchange of organochlorine pesticides along the Aba profile, east of the Tibetan Plateau, western China
Hongxia LIU1,2, Shihua QI1, Dan YANG3, Ying HU1, Feng LI1, Jia LIU1, Xinli XING1()
1. State Key Laboratory of Biogeology and Environmental Geology, School of Environmental Studies, China University of Geosciences, Wuhan 430074, China; 2. Hubei Key Laboratory of Mine Environmental Pollution Control & Remediation, School of Environmental Science and Engineering, Hubei Polytechnic University, Huangshi 435003, China; 3. Faculty of Engineering, China University of Geosciences, Wuhan 430074, China
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Abstract

Mianzhu—Aba profile, east of the Tibetan Plateau, was selected to study the occurrence of organochlorine pesticides (OCPs) along an altitudinal gradient. Dichlorodiphenyltrichloroethanes (DDTs), hexachlorocyclohexanes (HCHs) and Aldrin, Dieldrin and Endrin (Drins) in surface soils were detected in winter (March) and summer (July). Soil concentrations (ng·g-1, dw) in winter and summer ranged as follws: DDTs, 0.37–179.16 and 0.32–42.57; HCHs, 0.14–10.76 and 0.55–32.71; Drins, N.D–3.99 and 0.02–6.93, respectively. Main soil OCPs were p,p′-DDT, p,p′-DDE, β-HCH and Drins, among which Drins were rarely reported in current literature of the Tibetan Plateau. Higher OCP concentrations in the profile were attributed close to the agricultural fields of the Sichuan Basin, current lindane and non-dicofol DDTs inputs, and also long-range atmospheric transport from abroad. Soil OCP concentrations underwent obvious seasonal variation, with higher DDTs in winter and higher HCHs and Drins in summer. It may be caused by climatic conditions, summer monsoon type, and physico-chemical properties of such contaminants. Though “rest” phenomenon occurred in some sampling sites, HCHs and Drins showed an increasing trend with increasing altitude, while DDTs showed an evident decrease with increasing altitude. The altitudinal distributions of OCPs were all consistent with previous findings in other mountainous regions. A primary fugacity analysis on OCPs soil-air exchange indicated that the profile may be secondary sources for HCHs and Endrin. As with Aldrin, Dieldrin, and DDTs, the profile may be both secondary sources and sinks.

Key wordsorganochlorine pesticides (OCPs)    seasonal variation    altitudinal pattern    soil-air exchange    Mian-zhu—Aba profile    east of the Tibetan Plateau
收稿日期: 2013-06-03      出版日期: 2013-12-05
Corresponding Author(s): XING Xinli,Email:xingxinli5300225@163.com   
 引用本文:   
. Soil concentrations and soil-air exchange of organochlorine pesticides along the Aba profile, east of the Tibetan Plateau, western China[J]. Frontiers of Earth Science, 0, (): 395-405.
Hongxia LIU, Shihua QI, Dan YANG, Ying HU, Feng LI, Jia LIU, Xinli XING. Soil concentrations and soil-air exchange of organochlorine pesticides along the Aba profile, east of the Tibetan Plateau, western China. Front Earth Sci, 0, (): 395-405.
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https://academic.hep.com.cn/fesci/CN/10.1007/s11707-013-0404-9
https://academic.hep.com.cn/fesci/CN/Y0/V/I/395
Fig.1  
AreaSite No.Altitude/mGeographic informationAverage soil and air temperature/°C
Winter (March)Summer (July)
Mianzhu cityB001588E:104°13′25.4" N:31°18′31.6″12.5/16.524.4/28.0
Maoxian of Aba PrefectureB0021,410E:103°40′59.8″ N:31°32′12.6″6.5/8.020.0/23.0
Maoxian of Aba PrefectureB0031,710E:103°39′53.9″ N:31°49′47.3″8.0/10.019.8/25.5
Heishui county of Aba PrefectureB0041,840E:103°25′02.9″ N:31°56′39.9″2.0/8.019.0/24.0
Heishui county of Aba PrefectureB0052,190E:103°07′01.4″ N:32°04′08.9″3.2/6.019.0/22.4
Heishui county of Aba PrefectureB0062,690E:102°48′39.3″ N:32°06′05.6″-0.2/-3.415.2/16.0
Hongyuan county of Aba PrefectureB0073,620E:102°29′45.1″ N:32°12′37.8″1.4/6.817.8/20.0
Hongyuan county of Aba PrefectureB0083,578E:102°21′57.5″ N:32°26′45.2″0.1/-6.014.4/17.0
Aba county of Aba PrefectureB0093,320E:102°03′09.4″ N:32°44′26.1″2.5/6.019.8/24.4
Aba county of Aba PrefectureB0103,490E:101°59′24.2″ N:32°51′42.3″1.0/-8.214.2/16.5
Aba county of Aba prefectureB0113,320E:101°43′01.1″ N:32°54′07.9″0.4/-3.817.5/20.0
Tab.1  
OCPWinter (March)Summer (July)
Range/(ng·g-1)Mean/(ng·g-1)R2 cRange/(ng·g-1)Mean/(ng·g-1)R2 dKoae
α-HCH0.07-0.540.230.130.03-0.930.280.022.9×107
β-HCHN.D b-10.010.91- d0.35-11.827.250.024.4×108
γ-HCHN.D b-0.500.05- d0.01-0.230.080.375.6×107
δ-HCHN.D b-1.430.340.07N.D b-0.420.120.02- d
HCHs a0.14-10.761.530.020.55-32.717.730.03- d
p,p-DDT0.01-83.1110.980.100.19-14.142.580.086.4×109
o,p-DDTN.D b-4.430.40- d0.01-1.210.260.012.8×109
p,p-DDDN.D b-6.531.300.320.03-2.600.500.201.2×1010
p,p’-DDE0.17-85.099.810.170.02-26.283.750.234.9×109
DDTs a0.37-179.1622.490.150.32-42.577.090.18- d
AldrinN.D b-0.140.02- d0.01-4.910.730.131.2×108
DieldrinN.D b-0.250.03- dN.D b-0.250.040.257.8×108
EndrinN.D b-3.600.40- d0.01-4.610.630.081.3×108
Drins aN.D b-3.990.450.020.02-6.931.390.18- d
OCPs a0.51-181.6324.470.111.20-47.2216.210.01- d
Tab.2  
Mountainous regionHCHsDDTsAldrinDieldrinEndrinRef.
Taurus, Turkey0.5812.170.010.140.02Turgut et al., 2012
Andossi plateau, Italy0.3834.16- a- a- aTremolada et al., 2011
Pico de Teide, Spain- a5.40- a- a- aRibes et al., 2002
Pyrenees, Europe0.142.55- a- a- aGrimalt et al., 2004
Tibet, China0.06-0.850.01-7.70- a- a- aWang et al., 2012
Wolong, China0.640.64- a- a- aZheng et al., 2009
Revelstoke, western Canada2.87- a- a0.61- aDaly et al., 2007
Yoho, western Canada1.08- a- a1.79- aDaly et al., 2007
Oberservation, western Canada0.45- a- a0.23- aDaly et al., 2007
Zhejiang, China- a- a0.70-8.500.34-5.00- aZhang et al., 2012
Alps, Europe- a- a- a0.40-6.00- aKirchner et al., 2009
Aba profile, China1.5322.490.020.030.40This study in winter
Aba profile, China7.737.090.730.040.63This study in summer
Tab.3  
Fig.2  
Fig.3  
Fig.4  
Fugacity equationFugacity/PaC/( mol·m-3)T/K bOther Parameters
fs=CsRT/0.411ФomKoafs is fugacity in soilCs is soil concentrationaT is the average soil temperatureR is 8.31 Pa m3/(mol·K);Фom is 1.7 times TOC c;Koa is octanol-air partition coefficient of compound d
fa=CaRTfa is fugacity in airCa is air concentrationT is the average air temperature
fs/faThe fs/fa>1 indicates net volatilization from the soil to air
The fs/fa<1 indicates net deposition from air to soil
The fs/fa ~1 indicates equilibrium
Tab.4  
Fig.5  
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