Correlation of radon anomalies with microseismic events in Kangra and Chamba valleys of N-W Himalaya
Correlation of radon anomalies with microseismic events in Kangra and Chamba valleys of N-W Himalaya
| dc.creator | Virk, H. S.; Department of Physics, Guru Nanak Dev University, Amritsar-143005, India. | |
| dc.creator | Walia, Vivek | |
| dc.creator | Sharma, Anand Kumar | |
| dc.creator | Kumar, Naresh | |
| dc.creator | Kumar, Rajiv | |
| dc.date | 2012-05-07 | |
| dc.date.accessioned | 2018-03-16T15:54:43Z | |
| dc.date.available | 2018-03-16T15:54:43Z | |
| dc.identifier | http://ojs.unam.mx/index.php/geofisica/article/view/39877 | |
| dc.identifier.uri | http://repositorioslatinoamericanos.uchile.cl/handle/2250/1203547 | |
| dc.description | El monitoreo de radón en Palampur y Dalhousie, en los valles de Kangra y Chamba, utiliza la emanometría por medicióndiscreta de radón desde 1992, dentro del programa de Sismicidad del Himalaya del gobierno de la India. Se observa una correlaciónen ambas regiones investigadas con el número de microtemblores registrados por el Departamento de Meteorología de la India enel período 1992-1997. Se estudió el efecto de parámetros meteorológicos (temperatura, precipitación, humedad y velocidad delviento) sobre el nivel de radón. En la estación de Palampur se presenta correlación positiva de los niveles de radón con la temperatura,la precipitación y la humedad, y negativa con la velocidad del viento. | es-ES |
| dc.description | Radon monitoring was carried out at Palampur and Dalhousie stations in Kangra and Chamba valleys using emanometry fordiscrete measurements of time-series radon data since 1992 under Himalayan Seismicity programme of Government of India. Thecorrelation of radon data with micro-earthquakes recorded by Indian Meteorological Department (IMD) network during the timewindow 1992-1997 shows a rising trend both in microseismicity as well as radon in Kangra and Chamba valleys of N-W Himalayanregion under investigation.The effect of meteorological parameters (temperature, rainfall, humidity and wind velocity) on radon emanation was studied.The correlation co-efficients of radon data and the meteorological parameters recorded at Palampur suggest that temperature,rainfall and humidity have positive correlation, whereas wind velocity has negative correlation with radon. | en-US |
| dc.format | application/pdf | |
| dc.language | spa | |
| dc.publisher | Instituto de Geofísica | es-ES |
| dc.relation | http://ojs.unam.mx/index.php/geofisica/article/view/39877/36293 | |
| dc.source | Geofísica Internacional; Vol 39, No 3 (2000) | es-ES |
| dc.source | 0016-7169 | |
| dc.subject | Radón, anomalías, emanometría, alpha-logger, microsismos, precursores. | es-ES |
| dc.subject | Radon, anomalies, emanometry, alpha-logger, microseismicity, precursor. | en-US |
| dc.title | Correlation of radon anomalies with microseismic events in Kangra and Chamba valleys of N-W Himalaya | en-US |
| dc.title | Correlation of radon anomalies with microseismic events in Kangra and Chamba valleys of N-W Himalaya | es-ES |
| dc.type | Artículos de revistas | |
| dc.type | Artículos de revistas |