| dc.creator |
AKKURT, İskender |
|
| dc.creator |
Kulali, F. |
|
| dc.date |
2015-07-31T21:00:00Z |
|
| dc.date.accessioned |
2020-10-06T09:35:51Z |
|
| dc.date.available |
2020-10-06T09:35:51Z |
|
| dc.identifier |
286ebb4e-f2b3-45e2-9321-7008656695f7 |
|
| dc.identifier |
10.12693/aphyspola.128.b-445 |
|
| dc.identifier |
https://avesis.sdu.edu.tr/publication/details/286ebb4e-f2b3-45e2-9321-7008656695f7/oai |
|
| dc.identifier.uri |
http://acikerisim.sdu.edu.tr/xmlui/handle/123456789/55932 |
|
| dc.description |
Radon is an inert gas produced by the radioactive decay of radium with a half-life of 3.81 days. Radon is the largest source of natural ionizing radiation and every 2.6 km(2) of surface soil, to a depth of 15 cm, contains approximately 1 gram of radium, which releases radon in small amounts to the atmosphere. On a global scale, it is estimated that 91 TBq of radon are released from soil annually. In this work, the radon concentration in soil gas, which is transported from soil (1 m depth), is measured at five points in Pamukkale and its neighbourhood. |
|
| dc.language |
eng |
|
| dc.rights |
info:eu-repo/semantics/closedAccess |
|
| dc.title |
Investigation of Radon Concentrations in Pamukkale-Turkey |
|
| dc.type |
info:eu-repo/semantics/article |
|