2014
DOI: 10.1016/j.apgeochem.2014.09.018
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Natural 222 Rn and 220 Rn indicate the impact of the Water–Sediment Regulation Scheme (WSRS) on submarine groundwater discharge in the Yellow River estuary, China

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Cited by 28 publications
(11 citation statements)
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“…High salinity SGD has also been shown in some deltas. For example, Xu et al (2013Xu et al ( , 2014 used radium isotopes to quantify SGD fluxes in the Yellow River Delta. They estimated a SGD flux of 1.3 × 10 9 m 3 d −1 with a range of 2.8 × 10 8 -3.0 × 10 9 m 3 d −1 .…”
Section: Geophysical Processesmentioning
confidence: 99%
“…High salinity SGD has also been shown in some deltas. For example, Xu et al (2013Xu et al ( , 2014 used radium isotopes to quantify SGD fluxes in the Yellow River Delta. They estimated a SGD flux of 1.3 × 10 9 m 3 d −1 with a range of 2.8 × 10 8 -3.0 × 10 9 m 3 d −1 .…”
Section: Geophysical Processesmentioning
confidence: 99%
“…7 (B1-T and B1-S)) appears to be a reflection of these fresh SGD inputs, although hyperpycnal flows could have the same characteristics (Wright et al 1986) and we cannot necessarily exclude this possibility. However, low dissolved oxygen and low turbidity were also found in this bottom water mass, less than one half meter above the seabed, demonstrating that the source of this bottom water mass was fresh SGD rather than hyperpycnal flows (Xu et al 2014). Typical temperature and salinity profiles at site C2 (Fig.…”
Section: Influence Of the Wsrs On Sgdmentioning
confidence: 97%
“…Such drastic but controlled conditions present during a WSRS period provide a natural laboratory to address discharge effects on mixing, SGD, and other processes. Previous SGD studies in the Yellow River estuary showed a relatively significant groundwater flux compared with river discharge during non-WSRS periods (Taniguchi et al 2008;Peterson et al 2008b;Xu et al 2013), then Xu et al (2014) qualitatively described an increase of SGD flux during the WSRS period. However, there has been no quantitative assessment of the impact of the WSRS, concerning the variation of hydrodynamics and SGD fluxes into the estuary.…”
Section: Introductionmentioning
confidence: 92%
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“…Since 1996, natural radioactive isotopes Ra and Rn were widely used as tracers to estimate SGD in large scale areas ( Gu et al, 2012;Lee et al, 2012;Moore, 1996Moore, , 2007Moore and Oliveira, 2008;Wang et al, 2015;Xu et al, 2014) . Seepage meters were also used to estimated SGD at local area, such as manual seepage instrument developed by Cable et al ( 1997 ) , heat pulse seepage meter developed by Taniguchi and Fukuo (1993) and ultrasonic flow meter developed by Paulsen et al (2001) .…”
Section: Introductionmentioning
confidence: 99%