Investigating the effects of groundwater level changes on GNSS observations in the Konya Closed Basin
| dc.contributor.author | Erdoğan, Hediye | |
| dc.contributor.author | Oktar, Osman | |
| dc.contributor.author | Gezgin, Cemil | |
| dc.contributor.author | Poyraz, F. | |
| dc.contributor.author | Arslan, N. | |
| dc.contributor.author | Yılmaztürk, F. | |
| dc.date.accessioned | 2022-02-23T10:58:25Z | |
| dc.date.available | 2022-02-23T10:58:25Z | |
| dc.date.issued | 2022 | |
| dc.department | Mühendislik Fakültesi | |
| dc.description.abstract | The Konya Closed Basin (KCB), inhabited by approximately 4 million people, has a semi-arid climate and has been an important agricultural and economic production area with its fertile alluvial soils. In recent years, groundwater use as a primary source in the intense need for irrigation due to climate change, drought, and wrong agricultural policies triggered land subsidence in the basin by causing the aquifer system compaction. In this study, the effects of groundwater level changes obtained from groundwater monitoring stations on the positions of continuously operating GNSS stations located in KCB were investigated by time series analysis. As a result of trend component analyses of time series processed based on the ITRF08 fixed frame, it was determined that the horizontal positions of stations in this region were moving in the northeast direction (18.74 mm/year). For the up coordinates, while stations ANRK, KLUU, and NIGD had movements 0.56 mm/year in the up direction, the other stations moved in the down direction. The vertical movement of the KNY1 station based on 560-day data was in the down (-) direction, with an annual movement of 70.96 mm, and this was the maximum movement or velocity compared to the other stations in this region. The trend analysis of 19 wells revealed linear groundwater level changes in the down direction with a mean value of-39.22 cm/year. The decrease in the water level of the wells in the Konya Closed Basin was statistically significant for the majority of the wells and at meter level in some wells. | |
| dc.identifier.doi | 10.15446/esrj.v25n4.92490 | |
| dc.identifier.endpage | 414 | en_US |
| dc.identifier.issn | 1794-6190 | |
| dc.identifier.issue | 4 | en_US |
| dc.identifier.scopusquality | Q3 | |
| dc.identifier.startpage | 404 | en_US |
| dc.identifier.uri | https:/dx.doi.org/10.15446/esrj.v25n4.92490 | |
| dc.identifier.uri | https://hdl.handle.net/20.500.12451/9214 | |
| dc.identifier.volume | 25 | en_US |
| dc.indekslendigikaynak | Scopus | |
| dc.language.iso | en | |
| dc.publisher | Universidad Nacional de Colombia | |
| dc.relation.ispartof | Earth Sciences Research Journal | |
| dc.relation.publicationcategory | Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı | |
| dc.rights | info:eu-repo/semantics/openAccess | |
| dc.subject | Fast Fourier Transform | |
| dc.subject | GNSS | |
| dc.subject | Groundwater Level | |
| dc.subject | Konya Closed Basin | |
| dc.subject | Time Series Analysis | |
| dc.title | Investigating the effects of groundwater level changes on GNSS observations in the Konya Closed Basin | |
| dc.title.alternative | Investigación de los efectos del cambio en el nivel de aguas subterráneas a partir de observaciones de sistemas globales de navegación por satélite en la Cuenca de Konya, Turquía | |
| dc.type | Article |
