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Variability of dissolved CO2 in the Pang and Lambourn Chalk rivers.

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Variability of dissolved CO2 in the Pang and Lambourn Chalk rivers. / Griffiths, J.; Nutter, J.; Binley, Andrew et al.
In: Hydrology and Earth System Sciences, Vol. 11, No. 1, 17.01.2007, p. 328-339.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Griffiths, J, Nutter, J, Binley, A, Crook, N, Young, A & Pates, J 2007, 'Variability of dissolved CO2 in the Pang and Lambourn Chalk rivers.', Hydrology and Earth System Sciences, vol. 11, no. 1, pp. 328-339. <http://www.hydrol-earth-syst-sci.net/11/328/2007/>

APA

Vancouver

Griffiths J, Nutter J, Binley A, Crook N, Young A, Pates J. Variability of dissolved CO2 in the Pang and Lambourn Chalk rivers. Hydrology and Earth System Sciences. 2007 Jan 17;11(1):328-339.

Author

Griffiths, J. ; Nutter, J. ; Binley, Andrew et al. / Variability of dissolved CO2 in the Pang and Lambourn Chalk rivers. In: Hydrology and Earth System Sciences. 2007 ; Vol. 11, No. 1. pp. 328-339.

Bibtex

@article{2ad2bd56ffa2431c978f63169c33d62b,
title = "Variability of dissolved CO2 in the Pang and Lambourn Chalk rivers.",
abstract = "This paper presents the results of a two-year field campaign to determine the spatial and temporal variability of groundwater interaction with surface waters in two Cretaceous Chalk catchments (the Pang and Lambourn) in the Upper Thames in Berkshire, UK, based on measurement of dissolved carbon dioxide (CO2). Average stream water concentrations of dissolved CO2 were up to 35 times the concentration at atmospheric equilibrium. Mean groundwater concentrations of 85 and 70 times the atmospheric equilibrium were determined from borehole water sampled in the Pang and Lambourn respectively. Diurnal and seasonal variation of in-stream concentration of dissolved CO2 is not significant enough to mask the signal from groundwater inputs.",
author = "J. Griffiths and J. Nutter and Andrew Binley and Nigel Crook and A. Young and J. Pates",
year = "2007",
month = jan,
day = "17",
language = "English",
volume = "11",
pages = "328--339",
journal = "Hydrology and Earth System Sciences",
issn = "1027-5606",
publisher = "Copernicus Gesellschaft mbH",
number = "1",

}

RIS

TY - JOUR

T1 - Variability of dissolved CO2 in the Pang and Lambourn Chalk rivers.

AU - Griffiths, J.

AU - Nutter, J.

AU - Binley, Andrew

AU - Crook, Nigel

AU - Young, A.

AU - Pates, J.

PY - 2007/1/17

Y1 - 2007/1/17

N2 - This paper presents the results of a two-year field campaign to determine the spatial and temporal variability of groundwater interaction with surface waters in two Cretaceous Chalk catchments (the Pang and Lambourn) in the Upper Thames in Berkshire, UK, based on measurement of dissolved carbon dioxide (CO2). Average stream water concentrations of dissolved CO2 were up to 35 times the concentration at atmospheric equilibrium. Mean groundwater concentrations of 85 and 70 times the atmospheric equilibrium were determined from borehole water sampled in the Pang and Lambourn respectively. Diurnal and seasonal variation of in-stream concentration of dissolved CO2 is not significant enough to mask the signal from groundwater inputs.

AB - This paper presents the results of a two-year field campaign to determine the spatial and temporal variability of groundwater interaction with surface waters in two Cretaceous Chalk catchments (the Pang and Lambourn) in the Upper Thames in Berkshire, UK, based on measurement of dissolved carbon dioxide (CO2). Average stream water concentrations of dissolved CO2 were up to 35 times the concentration at atmospheric equilibrium. Mean groundwater concentrations of 85 and 70 times the atmospheric equilibrium were determined from borehole water sampled in the Pang and Lambourn respectively. Diurnal and seasonal variation of in-stream concentration of dissolved CO2 is not significant enough to mask the signal from groundwater inputs.

M3 - Journal article

VL - 11

SP - 328

EP - 339

JO - Hydrology and Earth System Sciences

JF - Hydrology and Earth System Sciences

SN - 1027-5606

IS - 1

ER -