1 / 4

232 Th 228 Ra

Estimate Submarine Groundwater Discharge (SGD)to the Atlantic Ocean. 232 Th 228 Ra. half life = 5.7 years l = 0.12 yr -1. Procedure:. 1. Measure inventory of 228 Ra in upper km of Atlantic Ocean. Flux 228 Ra = Inventory x l 2. Subtract riverine and sediment fluxes.

nitesh
Download Presentation

232 Th 228 Ra

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Estimate Submarine Groundwater Discharge (SGD)to the Atlantic Ocean 232Th 228Ra half life = 5.7 years l = 0.12 yr-1 Procedure: 1. Measure inventory of 228Ra in upper km of Atlantic Ocean. Flux 228Ra = Inventory x l 2. Subtract riverine and sediment fluxes. 3. Estimate 228Ra in SGD. TTO 1981-1989 228Ra flux (atoms) SGD Flux = [228Ra]SGD (at/L) Bob Key Princeton

  2. Distribution of 228Ra in SGD (226 samples) median mean Median = 6.5 x 106 at/L Mean = 17 x 106 at/L (3.9 dpm/L) (1.5 dpm/L)

  3. Total 228Ra Inventory = 2.9 x 1024 atoms Decay = 3.5 x 1023 at/yr River flux = 0.3 x 1023 at/yr Sed. flux = 1.3 x 1023 at/yr SGD flux = 1.9 x 1023 at/yr TTO 1981-1989 Mean 228Ra in SGD = 17 x 106 at/L (3.9 dpm/L) Median 228Ra in SGD = 6.5 x 106 at/L (1.5 dpm/L) SGD flux = 1-3 x 1016 L/yr River flux = 2.4 x 1016 L/yr 40-120% of the river water flux; probably >>river metal, nut, C flux

More Related