Zobrazeno 1 - 9
of 9
pro vyhledávání: '"John B. Ong"'
Publikováno v:
Water Resources Research. 50:8281-8299
Models of dual-domain mass transfer (DDMT) are used to explain anomalous aquifer transport behavior such as the slow release of contamination and solute tracer tailing. Traditional tracer experiments to characterize DDMT are performed at the flow pat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5e9dfedea4a06fca5e9dd87989021832
https://doi.org/10.1002/2014wr015880
https://doi.org/10.1002/2014wr015880
Autor:
Charles F. Harvey, Mason Stahl, M. H. Tarek, A. van Geen, J.A. Anderson, Carole D. Johnson, A.B.M. Badruzzaman, John B. Ong, John W. Lane
Publikováno v:
Groundwater. 52:195-200
We apply fluid-replacement logging in arsenic-contaminated regions of Bangladesh using a low-cost, down-well fluid conductivity logging tool to detect leaks in the cased section of wells. The fluid-conductivity tool is designed for the developing wor
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::96824b3634d006ccb5d948b17f452527
https://doi.org/10.1111/gwat.12200
https://doi.org/10.1111/gwat.12200
Publikováno v:
Water Resources Research. 49:5615-5630
[1] Anomalous solute transport, modeled as rate-limited mass transfer, has an observable geoelectrical signature that can be exploited to infer the controlling parameters. Previous experiments indicate the combination of time-lapse geoelectrical and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::480a925cac2b30cc3278b2b47690d25a
https://doi.org/10.1002/wrcr.20397
https://doi.org/10.1002/wrcr.20397
Publikováno v:
Hydrogeology Journal. 20:1483-1495
Lake–groundwater interactions exhibit a complex three-dimensional (3D) structure that is seldom studied. The utility of waterborne electrical resistivity (ER) surveys is explored for characterization of 3D groundwater flow and solute transport patt
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::45346972beaa7832865cc2671abe9c7a
https://doi.org/10.1007/s10040-012-0891-x
https://doi.org/10.1007/s10040-012-0891-x
Publikováno v:
Advances in Mathematics of Communications. 5:1-10
Elliptic curves over finite fields have applications in public key cryptography. A Koblitz curve is an elliptic curve $E$ over $\mathbb F$2; the group $E(\mathbb F$2n$)$ has convenient features for efficient implementation of elliptic curve cryptogra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1f7f79122896df897238dce8a05d14c3
https://doi.org/10.3934/amc.2011.5.1
https://doi.org/10.3934/amc.2011.5.1
Publikováno v:
Hydrogeology Journal. 18:1539-1545
A frequency-domain electromagnetic (FDEM) survey can be used to select locations for the more quantitative and labor-intensive electrical resistivity surveys. The FDEM survey rapidly characterized the groundwater-flow directions and configured the sa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b1dc918b553204bec3b5053c890d11c2
https://doi.org/10.1007/s10040-010-0617-x
https://doi.org/10.1007/s10040-010-0617-x
Publikováno v:
Journal of Hydrology. 371:22-30
Summary We investigate the conditions and criteria for identifying flow regimes in shallow groundwater-dominated lakes in arid environments. Relying on regional and local water-table configurations, we develop a steady-state model of lake-aquifer sys
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a9538ea700bbb65789d7d86a78b45b0c
https://doi.org/10.1016/j.jhydrol.2009.03.012
https://doi.org/10.1016/j.jhydrol.2009.03.012
Publikováno v:
Journal of Geophysical Research: Earth Surface. 117
[1] Emissions of salt dust from the shores of saline lakes significantly impact lake chemistry, air quality, transportation, human health, and climate. Quantitative methods for assessing these emissions, however, are still in the developmental stage.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4e2bce68eca8852590b36a989bae8a89
https://doi.org/10.1029/2011jf002107
https://doi.org/10.1029/2011jf002107
Autor:
John B. Ong, Vitaly A. Zlotnik
Publikováno v:
Ground water. 49(2)
Potentiomanometers (PMs) are commonly used to determine flux directions across interfaces between surface waters and aquifers. We describe a complementary function: estimating small-scale hydraulic conductivity (K) in a lakebed, using the constant-he
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::aeae0fd680c786cc78367f38b16cb9c9
https://pubmed.ncbi.nlm.nih.gov/20497483
https://pubmed.ncbi.nlm.nih.gov/20497483