Hydrogeological Research for Groundwater in the Nashec Spring

Session

Civil Engineering, Infrastructure and Environment

Description

The "Sozi" spring is located in the northwestern part of the city of Prizren, south of the village of Nashec, and represents one of the most important sources of drinking water for the region. This karst spring originates from the stratified limestone formations of the Pashtrik massif, at an altitude of 312.0 meters above sea level. Traditionally, this spring has played a crucial role in the water supply of the area's inhabitants since the establishment of settlements around it. Considering the karst character and the pronounced dependence on atmospheric precipitation, its capacity is estimated to be approximately 120 l/s, while the usable capacity for irrigation purposes and drinking water supply to local communities is 60-70 l/s. As part of efforts to ensure a sustainable water supply, a series of infrastructural and technical interventions have been carried out over the years. Among the most important ones are the construction of the collection chamber in 1977, the installation of drainage pipes in 2000 and 2010, the rehabilitation of the pumping station in 2020, and investments in water catchment in 2022. Currently, this source provides a stable water supply for 14 villages in the Has region and the western part of Prizren. Technical improvements have contributed to the stabilization of pressure in the distribution network and increased supply efficiency, guaranteeing better coverage and higher quality of drinking water for the residents of the area.

Keywords:

Groundwater, Hydrogeological research, Sozi spring, Nashec, Karst spring, Water supply, Catchment

Proceedings Editor

Edmond Hajrizi

ISBN

978-9951-982-41-2

Location

UBT Kampus, Lipjan

Start Date

25-10-2025 9:00 AM

End Date

26-10-2025 6:00 PM

DOI

10.33107/ubt-ic.2025.65

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Oct 25th, 9:00 AM Oct 26th, 6:00 PM

Hydrogeological Research for Groundwater in the Nashec Spring

UBT Kampus, Lipjan

The "Sozi" spring is located in the northwestern part of the city of Prizren, south of the village of Nashec, and represents one of the most important sources of drinking water for the region. This karst spring originates from the stratified limestone formations of the Pashtrik massif, at an altitude of 312.0 meters above sea level. Traditionally, this spring has played a crucial role in the water supply of the area's inhabitants since the establishment of settlements around it. Considering the karst character and the pronounced dependence on atmospheric precipitation, its capacity is estimated to be approximately 120 l/s, while the usable capacity for irrigation purposes and drinking water supply to local communities is 60-70 l/s. As part of efforts to ensure a sustainable water supply, a series of infrastructural and technical interventions have been carried out over the years. Among the most important ones are the construction of the collection chamber in 1977, the installation of drainage pipes in 2000 and 2010, the rehabilitation of the pumping station in 2020, and investments in water catchment in 2022. Currently, this source provides a stable water supply for 14 villages in the Has region and the western part of Prizren. Technical improvements have contributed to the stabilization of pressure in the distribution network and increased supply efficiency, guaranteeing better coverage and higher quality of drinking water for the residents of the area.