Quantifying river gain and loss at regional scales
• Small-scale estimates of exchange flux cannot be extrapolated to regional scales. • Hydraulic gradient calculations can estimate flux over scales of 100s of metres. • Differential flow gauging is most useful in small rivers. • River chemistry allows regional scale estimates of river gain at a poin...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Cook, Peter G. [verfasserIn] |
|---|
| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Schlagwörter: |
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| Umfang: |
10 |
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| Übergeordnetes Werk: |
Enthalten in: Neighborhood resources associated with frailty trajectories over time among community-dwelling older adults in China - Liu, Huiying ELSEVIER, 2021, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:531 ; year:2015 ; pages:749-758 ; extent:10 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.jhydrol.2015.10.052 |
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| 520 | |a • Small-scale estimates of exchange flux cannot be extrapolated to regional scales. • Hydraulic gradient calculations can estimate flux over scales of 100s of metres. • Differential flow gauging is most useful in small rivers. • River chemistry allows regional scale estimates of river gain at a point in time. • Groundwater chemistry allows estimation of river loss. | ||
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• Small-scale estimates of exchange flux cannot be extrapolated to regional scales. • Hydraulic gradient calculations can estimate flux over scales of 100s of metres. • Differential flow gauging is most useful in small rivers. • River chemistry allows regional scale estimates of river gain at a point in time. • Groundwater chemistry allows estimation of river loss. |
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• Small-scale estimates of exchange flux cannot be extrapolated to regional scales. • Hydraulic gradient calculations can estimate flux over scales of 100s of metres. • Differential flow gauging is most useful in small rivers. • River chemistry allows regional scale estimates of river gain at a point in time. • Groundwater chemistry allows estimation of river loss. |
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• Small-scale estimates of exchange flux cannot be extrapolated to regional scales. • Hydraulic gradient calculations can estimate flux over scales of 100s of metres. • Differential flow gauging is most useful in small rivers. • River chemistry allows regional scale estimates of river gain at a point in time. • Groundwater chemistry allows estimation of river loss. |
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