Factors controlling excess radium in the Nakdong River estuary, Korea: Submarine groundwater discharge versus desorption from riverine particles

Marine Chemistry

Volumn 78, Issue 1, 2002, Pages 1-8

  Yang, Han Soeb ^a   Hwang, Dong Woon ^a   Kim, Guebuem ^b  

^a Pukyong National University   (South Korea)

^b Seoul National University   (South Korea)

Author keywords

Brackish water; Desorption; Estuary; Radium; River dam; Submarine groundwater discharge

Indexed keywords

BIOGEOCHEMISTRY; DISCHARGE; ESTUARINE CHEMISTRY; GROUNDWATER FLOW; RADIUM;

KOREA;

EID: 0036220412     PISSN: 03044203     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0304-4203(02)00004-X     Document Type: Article

References (20)

1. Radium in the Suwannee River and estuary: Spring and river input to the Gulf of Mexico
2. 226Ra behavior in the Pee Dee River-Winyah Bay estuary
3. 228Ra in the mixing zones of the Pee Dee River-Winyah Bay, Yangtze River and Delaware Bay estuaries
4. 226Ra to trace groundwater discharge into the Chesapeake
5. 228Ra in the Amazon River estuary
6. 228Ra in the mixing zones of the Mississippi and Atchafalaya Rivers: Indicators of groundwater input
7. 226Ra from river-borne sediments in the Hudson Estuary
8. 226Ra from estuarine and continental shelf sediments
9. Radium and radon in Charlotte Harbor estuary, Florida
10. Radium isotopes in Chesapeake Bay
11. 226Ra enrichment
12. High fluxes of radium and barium from the mouth of the Ganges-Brahmaputra River during low river discharge suggest a large groundwater source
13. The subterranean estuary: A reaction zone of ground water and sea water
14. 226Ra in the Mississippi river mixing zone
15. 210Po in the East China and Yellow Seas
16. Uranium-series mobilization and surface hydrology
17. Chemistry of uranium, thorium and radium isotopes in the Ganges-Brahmaputra river system: Weathering processes and fluxes to the bay of Bengal
18. Radium isotopes in coastal and open ocean surface waters of the western North Pacific
19. 226Ra during estuarine mixing in the Mullica River estuary, New Jersey, U.S.A.: A comparison between field observation and equilibrium calculation