4.7 Article

Using RFID and accelerometer-embedded tracers to measure probabilities of bed load transport, step lengths, and rest times in a mountain stream

期刊

WATER RESOURCES RESEARCH
卷 51, 期 9, 页码 7572-7589

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1002/2014WR016120

关键词

bed load transport; step lengths; rest times; hysteresis; anomalous dispersion

资金

  1. National Science Foundation [EAR 1053508]
  2. Geological Society of America student grant
  3. American Association of Petroleum Geologists student grant
  4. American Federation of Mineralogical Sciences student grant
  5. ConocoPhillips student grant
  6. University of Texas Jackson School student grant
  7. Directorate For Geosciences
  8. Division Of Earth Sciences [1053508] Funding Source: National Science Foundation

向作者/读者索取更多资源

We present new measurements of bed load tracer transport in a mountain stream over several snowmelt seasons. Cumulative displacements were measured using passive tracers, which consisted of gravel and cobbles embedded with radio frequency identification tags. The timing of bed load motion during 11 transporting events was quantified with active tracers, i.e., accelerometer-embedded cobbles. Probabilities of cobble transport increased with discharge above a threshold, and exhibited slight to moderate hysteresis during snowmelt hydrographs. Dividing cumulative displacements by the number of movements recorded by each active tracer constrained average step lengths. Average step lengths increased with discharge, and distributions of average step lengths and cumulative displacements were thin tailed. Distributions of rest times followed heavy-tailed power law scaling. Rest time scaling varied somewhat with discharge and with the degree to which tracers were incorporated into the streambed. The combination of thin-tailed displacement distributions and heavy-tailed rest time distributions predict superdiffusive dispersion.

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