Naturally Occurring Radon 222 as a Tracer for Streamflow Generation: Steady State Methodology and Field Example

Water Resources Research

Volumn 26, Issue 12, 1990, Pages 3065-3075

  Genereux, David P ^a   Hemond, Harold F ^a  

^a NONE

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0242515037     PISSN: 00431397     EISSN: 19447973     Source Type: Journal    
DOI: 10.1029/WR026i012p03065     Document Type: Article

References (54)

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2. Biodegradation and gas exchange of gaseous alkanes in model estuarine ecosystems
3. Geologic and hydrologic factors controlling radon‐222 in ground water in Maine
4. 222Rn transport across the earth‐air interface
5. Snowmelt runoff from measurements of tritium and oxygen 18
6. Partial area contributions to storm runoff in a small New England watershed
7. Dichlorodifluoromethane (Freon‐12) as a tracer for nitrous oxide release from a nitrogen‐enriched river
8. The role of organic acids in the acid‐base status of surface waters at Bickford Watershed, Massachusetts
9. Alkalinity and major ion budgets for a Massachusetts reservoir and watershed
10. 222Rn concentrations and variations in unconfined groundwater
11. 222Rn content of soil‐gas by liquid scintillation counting
12. Geologic controls and radon occurrence in New England
13. Water flux in soil and subsoil on a steep forested slope
14. Nitrate processing and watershed acid sensitivity
15. Comments on letters relating to “Role of subsurface flow in generating surface runoff, 2, Upstream source areas” by R. Allen Freeze
16. Moisture and energy conditions within a sloping soil mass during drainage
17. A comparison of chemical and isotopic hydrograph separation
18. Determination of the components of stormflow using water chemistry and environmental isotopes, Mattole River Basin, California
19. The purpose of uncertainty analysis
20. Measurements of the effects of atmospheric variables on radon‐222 flux and soil‐gas concentrations
21. 222Rn in the ground and a new physical model for the transport
22. Radon measurement in streams to determine location and magnitude of groundwater seepage
23. Application of flow models in an alpine catchment area using tritium and deuterium data
24. New insight into the runoff mechanism by environmental isotopes
25. Silica in soil solutions, 1, The form and concentration of dissolved silica in aqueous extracts of some soils
26. Streamflow generation in a forested watershed, New Zealand
27. Use of specific conductance and contact time relations for separating flow components in storm runoff
28. 222Rn concentrations in water with a commercial liquid scintillation counter
29. Reaeration coefficients of streams: State of the art
30. Laboratory studies of gas tracers for reaeration
31. Laboratory studies of gas tracers for reaeration: Closure
32. Springflood: Meltwater or groundwater
33. Factors affecting exhalation of radon from a gravelly sand loam
34. The role of groundwater in storm runoff
35. A conceptual model of watershed response to rainfall, developed through the use of oxygen‐18 as a natural tracer
36. Storm runoff generation in humid headwater catchments, 2, A case of hillslope and low‐order stream response
37. Laboratory studies of gas tracers for reaeration: Discussion
38. Tracer measurements of atmospheric reaeration, 1, Laboratory studies
39. Gas exchange rates for a first‐order stream determined with deliberate and natural tracers
40. Throughflow on hillslopes and its relation to the stream hydrograph
41. Measurements of the downslope flow of water in a soil
42. Reaeration studies on some New Zealand rivers using methyl chloride as a gas tracer