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Riparian control of stream-water chemistry: Implications for hydrochemical basin models

Research output: Contribution to Journal/Magazine › Journal article › peer-review

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Standard

Riparian control of stream-water chemistry: Implications for hydrochemical basin models. / Hooper, Richard P.; Aulenbach, Brent T.; Burns, Douglas A. et al.
In: IAHS-AISH Publication, Vol. 248, 01.12.1998, p. 451-458.

Research output: Contribution to Journal/Magazine › Journal article › peer-review

Harvard

Hooper, RP, Aulenbach, BT, Burns, DA, McDonnell, J, Freer, J, Kendall, C & Beven, K 1998, 'Riparian control of stream-water chemistry: Implications for hydrochemical basin models', IAHS-AISH Publication, vol. 248, pp. 451-458.

APA

Hooper, R. P., Aulenbach, B. T., Burns, D. A., McDonnell, J., Freer, J., Kendall, C., & Beven, K. (1998). Riparian control of stream-water chemistry: Implications for hydrochemical basin models. IAHS-AISH Publication, 248, 451-458.

Vancouver

Hooper RP, Aulenbach BT, Burns DA, McDonnell J, Freer J, Kendall C et al. Riparian control of stream-water chemistry: Implications for hydrochemical basin models. IAHS-AISH Publication. 1998 Dec 1;248:451-458.

Author

Hooper, Richard P. ; Aulenbach, Brent T. ; Burns, Douglas A. et al. / Riparian control of stream-water chemistry : Implications for hydrochemical basin models. In: IAHS-AISH Publication. 1998 ; Vol. 248. pp. 451-458.

Bibtex

@article{bb546a171baf4831b6bfd35f6b1b7b40,
title = "Riparian control of stream-water chemistry: Implications for hydrochemical basin models",
abstract = "End-member mixing analysis has been used to determine the hydrological structure for basin hydrochemical models at several catchments. Implicit in this use is the assumption that controlling end members have been identified, and that these end members represent distinct landscape locations. At the Panola Mountain Research Watershed, the choice of controlling end members was supported when a large change in the calcium and sulphate concentration of one of the end members was reflected in the stream water. More extensive sampling of groundwater and soil water indicated, however, that the geographic extent of the contributing end members was limited to the riparian zone. Hillslope solutions were chemically distinct from the riparian solutions and did not appear to make a large contribution to streamflow. The dominant control of the riparian zone on stream-water chemistry suggests that hydrological flow paths cannot be inferred from stream-water chemical dynamics.",
author = "Hooper, {Richard P.} and Aulenbach, {Brent T.} and Burns, {Douglas A.} and Jeffrey McDonnell and James Freer and Carol Kendall and Keith Beven",
year = "1998",
month = dec,
day = "1",
language = "English",
volume = "248",
pages = "451--458",
journal = "IAHS-AISH Publication",
issn = "0144-7815",

}

RIS

TY - JOUR

T1 - Riparian control of stream-water chemistry

T2 - Implications for hydrochemical basin models

AU - Hooper, Richard P.

AU - Aulenbach, Brent T.

AU - Burns, Douglas A.

AU - McDonnell, Jeffrey

AU - Freer, James

AU - Kendall, Carol

AU - Beven, Keith

PY - 1998/12/1

Y1 - 1998/12/1

N2 - End-member mixing analysis has been used to determine the hydrological structure for basin hydrochemical models at several catchments. Implicit in this use is the assumption that controlling end members have been identified, and that these end members represent distinct landscape locations. At the Panola Mountain Research Watershed, the choice of controlling end members was supported when a large change in the calcium and sulphate concentration of one of the end members was reflected in the stream water. More extensive sampling of groundwater and soil water indicated, however, that the geographic extent of the contributing end members was limited to the riparian zone. Hillslope solutions were chemically distinct from the riparian solutions and did not appear to make a large contribution to streamflow. The dominant control of the riparian zone on stream-water chemistry suggests that hydrological flow paths cannot be inferred from stream-water chemical dynamics.

AB - End-member mixing analysis has been used to determine the hydrological structure for basin hydrochemical models at several catchments. Implicit in this use is the assumption that controlling end members have been identified, and that these end members represent distinct landscape locations. At the Panola Mountain Research Watershed, the choice of controlling end members was supported when a large change in the calcium and sulphate concentration of one of the end members was reflected in the stream water. More extensive sampling of groundwater and soil water indicated, however, that the geographic extent of the contributing end members was limited to the riparian zone. Hillslope solutions were chemically distinct from the riparian solutions and did not appear to make a large contribution to streamflow. The dominant control of the riparian zone on stream-water chemistry suggests that hydrological flow paths cannot be inferred from stream-water chemical dynamics.

M3 - Journal article

AN - SCOPUS:0032313407

VL - 248

SP - 451

EP - 458

JO - IAHS-AISH Publication

JF - IAHS-AISH Publication

SN - 0144-7815

ER -