Facies Evolutions in the Playa of Hoz-e Soltan
محورهای موضوعی : فصلنامه علمی پژوهشی سنجش از دور راداری و نوری و سیستم اطلاعات جغرافیایی
Manijeh Ghahroudi
1
,
Khadijeh Alinoori
2
1 - Professor, Department of Physical Geography, Faculty of Earth Sciences Shahid BeheshtiUniversity, Iran.
2 - postdoctoral researcher, Department of Physical Geography, Faculty of Earth Sciences, Shahid Beheshti University, Iran.
کلید واژه: Hoz-e Soltan, Face, Deformation, Displacement.,
چکیده مقاله :
Hoz-e-Sultan's playa, being one of the lowest locations on the Iran plateau, is crucial to the region's climate equilibrium and ecological changes. As a result, studying the deformation and disturbance of facies induced by human interventions and climate change, as well as identifying equilibrium thresholds, is critical. In the present research, the amount of deformation and equilibrium thresholds were evaluated over a 5-year period using ASAR C-band radar images and the differential interferometry technique during 2004-2009. Comparing the results of radar images and playa facies in a short and medium-term temporal scale showed that the facies disturbances were increased and dynamic equilibrium was changed. Therefore, the total changes that occurred during 2004-2009 were -3.4, which the direction of non-equilibrium (negative) in the muddy facies in the north and (positive) were 5.3 in the clay facies in the west of the region. Playa had the most non-equilibrium during 2004-2005 and 2007-2008, while it had more stable conditions during 2004-2006 and 2008-2009. During 2004-2009, southern playa was in a state of relative equilibrium. The non-equilibrium range occasionally extends towards the north of the playa, and it has progressed on the facies of the northwestern boundary as a result of increased human interference.
Hoz-e-Sultan's playa, being one of the lowest locations on the Iran plateau, is crucial to the region's climate equilibrium and ecological changes. As a result, studying the deformation and disturbance of facies induced by human interventions and climate change, as well as identifying equilibrium thresholds, is critical. In the present research, the amount of deformation and equilibrium thresholds were evaluated over a 5-year period using ASAR C-band radar images and the differential interferometry technique during 2004-2009. Comparing the results of radar images and playa facies in a short and medium-term temporal scale showed that the facies disturbances were increased and dynamic equilibrium was changed. Therefore, the total changes that occurred during 2004-2009 were -3.4, which the direction of non-equilibrium (negative) in the muddy facies in the north and (positive) were 5.3 in the clay facies in the west of the region. Playa had the most non-equilibrium during 2004-2005 and 2007-2008, while it had more stable conditions during 2004-2006 and 2008-2009. During 2004-2009, southern playa was in a state of relative equilibrium. The non-equilibrium range occasionally extends towards the north of the playa, and it has progressed on the facies of the northwestern boundary as a result of increased human interference.
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