Relationship between Patterned Grounds Evolutions and Spatial and Temporal Changes in the Chemical Compounds of SAHL ABAD Playa Salt Flats (Case Study: Khorasan province)

Document Type : Research Paper

Author

Assistant Professor of Geomorphology, University of Payamenoor, Tehran, Iran

Abstract

The sensitive environment of Playa, as one of the largest mineral resources, has a special place in economic activities. Chemical compounds available in Playa are essential for soil which are used to fertilize agricultural soil. SAHL ABAD playa in the south Khorasan province, have special geomorphologic landscape by the presence of ephemeral saline lakes, wetlands, salt crusts, surface accumulations of salt and zones of pattern ground and it is always inhabited by mineral and agricultural exploitation. The issue of incorrect exploitation and excessive mineral resources of the Sahl Abad playa with the occurrence of abnormal changes in the playa geomorphology perspective can exacerbate the risks of wind erosion by increasing the sediment load. In this study, percent changes in some of the chemical compounds such as sodium chloride, sodium and gypsum in the playa were calculated with the aim of satellite data for two periods. Besides, using texture and pattern analysis of the PCA1, percent changes in the surface pattern grounds of the playa was calculated. Finally, we study the relationship between these two groups of changes in the playa surface. It was found that soil-surface salt accumulations are dominated by sodium chloride and gypsum and distribution of chemical soluble is not uniform across the playa landscape resulting in the variety form of pattern ground. Moreover, chemical compounds, are correlated with each other. There is positive relationship between percentage changes in patterned grounds and the percentage of changes in the chemical compounds at a significant level. The greatest effect on the chemical compounds studied on the evolution of pattern grounds of playa surfaces is related to changes in the concentration of sodium chemical composition with a correlation of about 0.35.

Extended Abstract

1-Introduction

Playa is a closed drainage system with a shallow water mass, which is strongly influenced by evaporation due to the drought conditions in its environment. The sensitive environment of Playa, as one of the largest mineral resources, has a special place in economic activities. Chemical compounds available in Playa are also essential for soil and are used to fertilize agricultural soil. SAHL ABAD playa in the south Khorasan province, have special geomorphologic landscape by the presence of ephemeral saline lakes, wetlands, salt crusts, surface accumulations of salt and zones of pattern ground and it is always inhabited by mineral and agricultural exploitation. The issue of incorrect exploitation and excessive mineral resources of the Sahl Abad playa with the occurrence of abnormal changes in the playa geomorphology perspective can exacerbate the risks of wind erosion by increasing the sediment load.

2-Materials and Methods

In this study, changes in the concentration of chemical compounds of playa surface as independent variables and morphological changes of pattern grounds are considered as dependent variables. Percent changes in the chemical compounds such as sodium chloride, sodium and gypsum in the playa were calculated with the aim of satellite data for two periods. Besides, using texture and pattern analysis of the PCA1, percent changes in the surface pattern grounds of the playa were calculated. Finally, we study the relationship between these two groups of changes in the playa surface.

3-Results and Discussion

It was found that soil-surface salt accumulations are dominated by sodium chloride and gypsum. Besides, the distribution of chemical soluble is not uniform across the playa landscape resulting in the various forms of patterned grounds. Furthermore, chemical compounds, are correlated with each other. There is positive relationship between percentage changes in patterned grounds and the percentage of changes in the chemical compounds at a significant level. The greatest effect on the chemical compounds studied on the evolution of pattern grounds of the playa surfaces is related to changes in the concentration of sodium chemical composition with a correlation of about 0.35. Therefore, the most unstable pattern grounds are found in the zones where sodium and sodium chloride chemical compounds predominate. In fact, the zones of the playa surface, covered by salt shells and masses, exposed and exhibited a few prominent patterns, are patterned grounds with the predominance of chemical compounds of sodium and sodium chloride in the region. These zones are considered in the group of patterned grounds with severe regional changes. The least correlation between chemical variables and texture of the pattern grounds is related to gypsum chemical compounds. Due to the low rainfall and humidity of the region and the less tendency for this chemical composition to the process of dissolving, the time required to create the most prominent pattern grounds with the presence of this chemical composition in the playa surface is provided. Therefore, in pattern grounds, with less changes or relatively stable of the playa surface, the chemical composition of gypsum is overcome, with the most significant patterns due to the presence of gypsum chemical composition.

4-Conclusion

The evaluation of pattern grounds according to the changes made in chemical compounds to detect environmental changes or other changes in the playa surface is an important issue that can indicate the desertification status and the severity of the risks of the expansion of the playa. In general, the results of this study indicate a correlation between the changes in the concentration of chemical compounds with the changes in the patterned areas of the study area. Investigating the chemical changes of the Sahl Abad playa surface indicates a slow and limited trend in the expansion of the playa during the study period. In these studies, data deficits are one of the most important problems, while the satellite data can be replaced by field observations if it is possible to provide reliable interpretations of the spectrum. Therefore, we can assess the relationship between the effective variables in the Playa expansion process, and given the fact that the process of satellite imaging is a sequential process, one can create relationships in previous studies in a region and with the advancements in technology, it instantly optimized.

 

Keywords


اشتوکلین، یوهان؛ افتخارنژاد، جمشید؛ هوشمندزاده، عبدالرحیم (1352) بررسی مقدّماتی زمین­شناسی در لوت مرکزی، خاور ایران، سازمان زمین­شناسی کشور، گزارش (22).
درویش­زاده، علی (1371) شرایط زمین­شناسی ایجاد کویرها و بیابان­های ایران، مجموعه­مقالات بررسی مسائل مناطق کویری ایران، انتشارات دانشگاه تهران، صص 186-179.
رضایی‌مقدم، محمدحسین؛ ثقفی، مهدی (1385) بررسی تحوّلات ژئومورفیک پلایای کهک، استان خراسان جنوبی براساس روش استفاده از تصاویر ماهواره‌ای و منطق فازی، جغرافیا و توسعه، 4 (8)، صص. 60-43.
رضایی‌مقدم، محمدحسین؛ ثقفی، مهدی (1383) طبقه­بندی و تحلیل مورفولوژی لندفرم­های زمین با استفاده از GIS و DEM، جغرافیا و برنامه­ریزی، 8 (17)، صص. 90-75.
رئیس‌السادات، سید ناصر؛ زرین‌کوب، محمدحسین؛ خطیب، محمدمهدی (1391) زمین‌ریخت‌شناسی و نحوة پیدایش پلایای سهل­آباد - خاور ایران، جغرافیا و توسعه، 10 (28)، صص. 132-115.
کلینسلی، دانیل (1381) کویرهای ایران و خصوصیات ژئومورفولوژیکی و پالئوکلیماتولوژی آن، ترجمة عباس پاشایی، انتشارات سازمان جغرافیایی نیروهای مسلّح، تهران.
محمدی، ملیحه (1394) آشکارسازی تغییرات واحدهای ژئومورفولوژی پلایاهای ایران مرکزی با استفاده از تصاویر ماهواره‌ای چندزمانه (گاوخونی، دق­سرخ، نمک قم، ابرکوه، میغان، طبس، سیرجان، جازموریان)، رسالة دکتری ژئومورفولوژی، استاد راهنما: عبدالله سیف، دانشکدة علوم جغرافیایی و برنامه‌ریزی، دانشگاه اصفهان.
Brabyan, L. (1998) GIS analysis of macro landform, Presented at the 10th Colloquium of the Spatial Information Research Center, University of Otago, New Zealand, 16-19 November, pp. 35-48.
Bryant, R. G. (2013) Recent advances in our understanding of dust source emission processes, Progress in Physical Geography, 37, pp. 397-421.
Darvishzadeh, A. (1992) Geological conditions of deserts and deserts of Iran, Collections of Issues of Desert Areas of Iran, Tehran University press, pp. 186-179 (In Persian).
Goodspeed, M. J., Winkworth, R. E. (1978) Fate and effect of runoff with special reference to arid and semi-arid plain lands, In: K. M. W. Howe’s (Ed.), Studies of the Australian arid zone: III. water in rangelands, 53-63, Proceedings of a Symposium Held at the Rangelands Research Unit, Alice Springs Field Centre, 15-18 October 1974, Melbourne, CSIRO Division of land resources management.
Goudie, A. S. (1991) Pans, Progress in Physical Geography: Earth and Environment, 15 (3), pp. 221-237.
Gutie´rrez-Elorza, M., Desir, M., Gutie´rrez-Santolalla, F., Marı´n, C. (2005) Origin and evolution of playas and blowouts in the semiarid zone of Tierra de Pinares (Duero Basin, Spain), Geomorphology, 72 (2), pp. 177-192.
Hall, A. (1995) Change detection, er mapper 5.0 applications, Earth Resource Mapping Pty. Ltd, pp. 47-57.
Howari, F. M., Goodell, P. C., Miyamoto, S. (2002) Spectral properties of salt crusts formed on saline soils, Environmental Quality, 31 (5), pp. 1453-1461.
Hubbard, B. E., Crowley, J. K. (2005) Mineral mapping on the Chilean–Bolivian Altiplano using Co-Orbital ALI, ASTER and hyperion imagery: Data dimensionality issues and solutions, Remote Sensing Environment, 99 (1-2), pp. 173-186.
Klinsley, D. (2002) The desert of Iran and geomorphological features and its palaeoclimatiligy. Translated by Abbas Pashaei, National geographical organization, Tehran (In Persian).
Mees, F. (1999) Distribution patterns of gypsum and kalistrontite in a dry lake basin of the Southwestern Kalahari (Omongwa Pan, Namibia), Earth Surface Processes and Landforms, 24 (8), pp. 731-744.
Milewski, R., Chabrillat, S., Behling, R. (2017) Analyses of recent sediment surface dynamic of a Namibian Kalahari salt pan based on multitemporal landsat and hyperspectral hyperion data, Remote Sensing, 9 (2), pp. 170-194.
Millington, A. C., Drake, N. A., Townshend, J. R. G., Quarmby, N. A., Settle, J. J., Reading, A. J. (1989) Monitoring salt playa dynamics using Thematic Mapper data, IEEE Transactions on Geoscience and Remote Sensing, 27 (6), pp. 754-761.
Mohammadi, M. (2015) Detection of changes in geomorphologic units of central Iran's playa using multi-temporal satellite imagery (Gavkhoni, Dagh-Sorkh, Salt Qom, Abarkuh, Mighan, Tabas, Sirjan, Jazmourian), Ph.D. thesis geomorphology, Supervisor: Abdullah Seif, Faculty of Geography and Planning, University of Esfahan (In Persian).
Montana, C. (1992) The colonization of bare areas in two phase mosaics of an arid ecosystem, The Journal of Ecology, 80 (2), pp. 315-327.
Neal, J. T. (1975) Playa surface features as indicators of environment. In: J. T. Neal (Ed.), Playas and Dried Lakes (pp.363-380), Stroudsburg, PA, USA: Dowden, Hutchinson & Ross.
Prospero, J. M., Ginoux, P., Torres, O., Nicholson, S. E., Gill, T. E. (2002) Environmental characterization of global sources of atmospheric soil dust identified with the NIMBUS 7 Total Ozone Mapping Spectrometer (TOMS) absorbing aerosol product, Reviews of Geophysics, 40 (1), pp. 2-31.
Raeis Alsadat, N., Zarinkoub, M. H., Khatib, M. M. (2012) Geomorphology and the way of the emergence of Sahl Abad playa - East of Iran, Geography and Development, 10 (28), pp. 132-115 (In Persian).
Reynolds, R. L., Yount, J. C., Reheis, M., Goldstein, H., Chavez, P., Fulton, R., Forester, R. M. (2007) Dust emission from wet and dry playas in the Mojave desert, USA, Earth Surface Processes and Landforms, 32 (12), pp. 1811-1827.
Rezaei Moghadam, M. H., Saghafi, M. (2004) Classification and analysis of land morphology using GIS and DEM, Geography and Planning, 8 (17), pp. 90-75 (In Persian).
Rezaei Moghadam, M. H., Saghafi, M. (2006) The research on the geomorphic evaluations of Kahak playa, South Khorasan province based on satellite imagery and fuzzy logic, Geography and Development, 4 (8), pp. 60-43 (In Persian).
Richards, J., Jia, X. (1999) Remote Sensing Digital Image Analysis: An Introduction, Berlin New York: Springer.
Rosen, M. R. (1994) The importance of groundwater in playas: a review of playa classifications and the sedimentology and hydrology of playas, In: M. R. Rosen (Ed.), Paleoclimate and basin evolution of playa systems, Geological Society of America Special Paper 289, Geological Society of America, (pp. 1-18), Boulder, CO.
Saghafi, M. (2017) Application of remote sensing indices for mapping salt affected areas by using field data methods, International Journal of Advanced and Applied Sciences, 4 (10), pp. 181-187.
Shaw, P. A., Bryant, R. G. (2011) Playas and salt lakes, In: D. S. G Thomas (Ed.), Arid Zone Geomorphology, (pp. 373-401), London, UK: John Wiley & Sons Ltd.
Stocklin, J., Eftekharnezhad, J., Houshmandzadeh, A. (1974) Basic study of geology in central Lut, East of Iran. Geological survey of Iran, Report (22) (In Persian).
Washington, R., Todd, M., Middleton, N. J., Goudie, A. S. (2003) Dust storm source areas determined by the total ozone monitoring spectrometer and surface observations, Annals of the Association of American Geographers, 93 (2), pp. 297-313.
White, K., Eckardt, F. (2006) Geochemical mapping of carbonate sediments in the Makgadikgadi basin, Botswana using moderate resolution remote sensing data, Earth Surface Processes and Landforms, 31, pp. 665-681.
White, L. P. (1969) Vegetation arcs in Jordan, The Journal of Ecology, 57 (2), pp. 461-464.
White, L. P. (1971) Vegetation stripes on sheet wash surfaces, The Journal of Ecology, 59. pp. 615-622.
Wickens, G. E., Collier, F. W. (1971) Some vegetation patterns in the republic of the Sudan, Geoderma, 6, pp. 43-59.
Worrall, G. A. (1960) Tree patterns in The Sudan. Journal of Soil Science, 11 (1), pp. 63-67.