دوره 8، شماره 16 - ( پاییز و زمستان 1396 )                   جلد 8 شماره 16 صفحات 131-123 | برگشت به فهرست نسخه ها


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(2018). Sediment source ascription in Vartavan catchment using composite fingerprint technique. jwmr. 8(16), 123-131. doi:10.29252/jwmr.8.16.123
URL: http://jwmr.sanru.ac.ir/article-1-909-fa.html
مصفایی جمال، اختصاصی محمدرضا، صالح‌پور جم امین، رجبی محمدرسول. منشایابی رسوبات آبی حوضه ورتوران قزوین با روش انگشت نگاری ترکیبی پ‍‍ژوهشنامه مديريت حوزه آبخيز 1396; 8 (16) :131-123 10.29252/jwmr.8.16.123

URL: http://jwmr.sanru.ac.ir/article-1-909-fa.html


چکیده:   (3375 مشاهده)
نخستین گام برنامه‌ریزی برای اجرای برنامه‌های حفاظت خاک، تشخیص منابع تولید رسوب می­باشد. به دلیل وجود مشکلات زیاد روش­های سنتی برای تعیین سهم منابع رسوب، روش انگشت­نگاری بعنوان جایگزینی مناسب مورد توجه محققین قرار گرفته است. هدف اصلی این تحقیق استفاده از تکنیک انگشت­نگاری ترکیبی برای تعیین سهم و اهمیت نسبی منابع رسوب حوزه ورتوان قزوین در تولید رسوب حوزه می­باشد. بدین منظور پس از تهیه نقشه دقیق واحدهای سنگ­شناسی حوزه، تعداد 66 نمونه از منابع رسوب و 9 نمونه از رسوبات خروجی حوزه برداشت و بر روی آنها دانه­بندی و تجزیه عنصری و کانی­شناسی انجام گردید. سپس واحدهای نه­گانه سنگ­شناسی با استفاده از روش تحلیل خوشه­ای به منابع سه­گانه آتشفشانی، رسوبی تبخیری (آهکی) و رسوبی تخریبی دسته­بندی گردید. با بکارگیری آزمون مقایسه میانگین­ها و تحلیل تابع تشخیص، سه ردیاب کادمیوم، سرب و کلسیت بعنوان ترکیب بهینه ردیاب‌ها تعیین شدند. خروجی مدل­های چندمتغیره ترکیبی نشان داد که در زیرحوزه کامان سهم واحدهای رسوبی تخریبی (مادستون قرمز، ماسه­سنگ قرمز، شیل ذغالی)، تبخیری (آهک شیلی، آهک اوربیتولین­دار، آهک با بین­لایه­های توف روشن) و آتشفشانی (توف تیره، آندزیت) به ترتیب برابر 4/63، 8/25 و 8/10 درصد، و در زیرحوزه موشقین به ترتیب برابر 2/36، 9/45 و 9/17 درصد می­باشد و در خروجی کل حوزه، سهم این واحدها به ترتیب برابر 6/47، 4/37 و 1/15 درصد می­باشد. اما اهمیت نسبی منابع رسوب که شاخصی است که عامل مساحت منابع مختلف در آن حذف شده است، در حوضه ورتوان و زیرحوضه­های آن بصورت رسوبی تخریبی > رسوبی تبخیری > آتشفشانی است.
متن کامل [PDF 2428 kb]   (1677 دریافت)    
نوع مطالعه: پژوهشي | موضوع مقاله: تخصصي
دریافت: 1396/11/10 | ویرایش نهایی: 1396/12/7 | پذیرش: 1396/11/10 | انتشار: 1396/11/10

فهرست منابع
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2. Collins, A. L., D. E. Walling, and G Leeks. J. L. 1997. Source type ascription for fluvial suspended sediment based on a quantitative composite fingerprinting technique. CATENA, 29(1): 1-27.
3. Collins, A.L and D.E. Walling. 2002. Selecting fingerprint properties for discriminating potential suspended sediment sources in river basins. Journal of Hydrology, 261: 218-244.
4. Collins, A.L and D.E. Walling. 2004. Documenting catchment suspended sediment sources: problems, approaches and prospects. Progress in Physical Geography, 28: 159–196.
5. Collins, A. L and D. E. Walling. 2007. Source type ascription for fluvial suspended sediment based on a quantitative composite fingerprinting technique. Geomorphology, 88(1): 120-138.
6. Fathizad, H., H. Karimi., M. Tavakoli. 2016. Role of sensitivity of erosion the geological formations at erosion rate and sediment yield (Case study: sub-basins of Doviraj river, Ilam province). Journal of Watershed Management Research 7(13): 193-208. (In Persian)
7. Feiznia, S., A. Mohammadi., M. Mohseni Saravi and F. Ghadimi Aross Mahalleh. 2007. Investigating effect of land use changes and geological formations sensibility to water erosion and sediment yield (Case study: Daryacheh - e – Namak). Journal of the Iranian Natural Resourses, 60(3): 811-828. (In Persian)
8. Hakimkhani, Sh and H. Ahmadi. 2008. Determining subbasins contributions to sediment yield using sediment fingerprinting method (Case study: Margan basin, Pouldasht). Journal of Agricultural Sciences and Natural Resources, 15,: 181-191. (In Persian)
9. Hakimkhani, Sh., H. Ahmadi and J.Ghayoumian. 2009. Determining erosion types contributions to the sediment yield using sediment fingerprinting method (Case study: Margan watershed). Iranian Journal of Soil and Waters Sciences, 19(1): 83-94. (In Persian)
10. Homauonfar, V., A. Khaledi Darvishan., S. H. R. Sadeghi. 2016. Effects of soil preparation for laboratorial erosion studies on surface runoff. Journal of Watershed Management Research 7(14), 60-68. (In Persian)
11. Klages, M.G and Y.P. Hsieh. 1975. Suspended solid carried by the Gallatin River of Southwestern Montana: II. Using mineralogy for inferring sources. Journal of Environmental Quality, 4, 68-73.
12. Kouhpeima, A., S. Feiznia. H. Ahmadi and S.A.A. Hashemi. 2011. Determining the ability of acid extractable metals as a fingerprint in sediment source discrimination. International Journal of Natural Resources and Marine Sciences, 1(2): 93-99.
13. Loughran, R.J and Campbell, B.L. 1995. The identification of catchment sediment sources. In: Foster, I.D.L., Gumell, A.M, B.W. Webb (Eds.). Sediment and Water Quality in River Catchments. Wiley, Chichester, 189-205.
14. Mosaffaie J., M. R. Ekhtesasi, M. T. Dastorani., H. R. Azimzadeh and M. A. Zare Chahuki, 2014. Temporal and spatial variation of the water erosion rate. Arabian journal of Geosciences. DOI: 10.1007/s12517-014-1628-z.
15. Mosaffaie, J and M. R. Ekhtesasi. 2016. Comparison of the relative sediment yield potential of lithological units using sediment grain color. Iran-watershed management science & engineering 10 (32): 51-58. (In Persian)
16. Mosaffaie, J and M. R. Ekhtesasi, (In press). Comparison of direct and indirect methods for sediment source tracing. Iran-watershed management science & engineering. (In Persian)
17. Nazari Samani, A., R.J. Wasson and A. Malekian. 2011. Application of multiple sediment fingerprinting techniques to determine the sediment source contribution of gully erosion: Review and case study from Boushehr province southwestern, Iran. Progress in Physical Geography, 35(3): 75-391.
18. Nosrati, K., G. Govers., H. Ahmadi., F. Sharifi., M.A. Amoozegar., R. Merckx and M. Vanmaercke. 2011. An exploratory study on the use of enzyme activities as sediment tracers: biochemical fingerprints? International Journal of Sediment Research, 26, 136-151.
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23. Wood, P.A. 1978. Fine-sediment mineralogy of source rocks and suspended sediment, rother catchment, West Sussex. Earth Surface Processes, 3(3): 255-263.
24. Yamani, M and N. Ebrahimkhani. 2010. Erosion vulnerability assessment through sedimentation alluvium formation of index case study: haji Arab basin (Qazvin province). Geography, 8(24): 69-86.
25. Carreras, N.M., T. Udelhoven Krein., Gallart. A., Iffly F, J.F., Ziebel, J., Hoffman, L., L. Pfister and D.E. Walling. 2010. The use of sediment coulor measured by reflectance spectrometry to determine sediment source: application to the Attert river catchment (Luxembourg). Journal of Hydrology, 382: 49-63. [DOI:10.1016/j.jhydrol.2009.12.017]
26. Collins, A. L., D. E. Walling, and G Leeks. J. L. 1997. Source type ascription for fluvial suspended sediment based on a quantitative composite fingerprinting technique. CATENA, 29(1): 1-27. [DOI:10.1016/S0341-8162(96)00064-1]
27. Collins, A.L and D.E. Walling. 2002. Selecting fingerprint properties for discriminating potential suspended sediment sources in river basins. Journal of Hydrology, 261: 218-244. [DOI:10.1016/S0022-1694(02)00011-2]
28. Collins, A.L and D.E. Walling. 2004. Documenting catchment suspended sediment sources: problems, approaches and prospects. Progress in Physical Geography, 28: 159-196. [DOI:10.1191/0309133304pp409ra]
29. Collins, A. L and D. E. Walling. 2007. Source type ascription for fluvial suspended sediment based on a quantitative composite fingerprinting technique. Geomorphology, 88(1): 120-138. [DOI:10.1016/j.geomorph.2006.10.018]
30. Fathizad, H., H. Karimi., M. Tavakoli. 2016. Role of sensitivity of erosion the geological formations at erosion rate and sediment yield (Case study: sub-basins of Doviraj river, Ilam province). Journal of Watershed Management Research 7(13): 193-208. (In Persian) [DOI:10.18869/acadpub.jwmr.7.13.208]
31. Feiznia, S., A. Mohammadi., M. Mohseni Saravi and F. Ghadimi Aross Mahalleh. 2007. Investigating effect of land use changes and geological formations sensibility to water erosion and sediment yield (Case study: Daryacheh - e - Namak). Journal of the Iranian Natural Resourses, 60(3): 811-828. (In Persian)
32. Hakimkhani, Sh and H. Ahmadi. 2008. Determining subbasins contributions to sediment yield using sediment fingerprinting method (Case study: Margan basin, Pouldasht). Journal of Agricultural Sciences and Natural Resources, 15,: 181-191. (In Persian)
33. Hakimkhani, Sh., H. Ahmadi and J.Ghayoumian. 2009. Determining erosion types contributions to the sediment yield using sediment fingerprinting method (Case study: Margan watershed). Iranian Journal of Soil and Waters Sciences, 19(1): 83-94. (In Persian)
34. Homauonfar, V., A. Khaledi Darvishan., S. H. R. Sadeghi. 2016. Effects of soil preparation for laboratorial erosion studies on surface runoff. Journal of Watershed Management Research 7(14), 60-68. (In Persian) [DOI:10.29252/jwmr.7.14.68]
35. Klages, M.G and Y.P. Hsieh. 1975. Suspended solid carried by the Gallatin River of Southwestern Montana: II. Using mineralogy for inferring sources. Journal of Environmental Quality, 4, 68-73. [DOI:10.2134/jeq1975.00472425000400010016x]
36. Kouhpeima, A., S. Feiznia. H. Ahmadi and S.A.A. Hashemi. 2011. Determining the ability of acid extractable metals as a fingerprint in sediment source discrimination. International Journal of Natural Resources and Marine Sciences, 1(2): 93-99.
37. Loughran, R.J and Campbell, B.L. 1995. The identification of catchment sediment sources. In: Foster, I.D.L., Gumell, A.M, B.W. Webb (Eds.). Sediment and Water Quality in River Catchments. Wiley, Chichester, 189-205.
38. Mosaffaie J., M. R. Ekhtesasi, M. T. Dastorani., H. R. Azimzadeh and M. A. Zare Chahuki, 2014. Temporal and spatial variation of the water erosion rate. Arabian journal of Geosciences. DOI: 10.1007/s12517-014-1628-z. [DOI:10.1007/s12517-014-1628-z]
39. Mosaffaie, J and M. R. Ekhtesasi. 2016. Comparison of the relative sediment yield potential of lithological units using sediment grain color. Iran-watershed management science & engineering 10 (32): 51-58. (In Persian)
40. Mosaffaie, J and M. R. Ekhtesasi, (In press). Comparison of direct and indirect methods for sediment source tracing. Iran-watershed management science & engineering. (In Persian)
41. Nazari Samani, A., R.J. Wasson and A. Malekian. 2011. Application of multiple sediment fingerprinting techniques to determine the sediment source contribution of gully erosion: Review and case study from Boushehr province southwestern, Iran. Progress in Physical Geography, 35(3): 75-391. [DOI:10.1177/0309133311401643]
42. Nosrati, K., G. Govers., H. Ahmadi., F. Sharifi., M.A. Amoozegar., R. Merckx and M. Vanmaercke. 2011. An exploratory study on the use of enzyme activities as sediment tracers: biochemical fingerprints? International Journal of Sediment Research, 26, 136-151. [DOI:10.1016/S1001-6279(11)60082-6]
43. Peart, M.R and D.E. Walling. 1988. Techniques for establishing suspended sediment sources in two drainage basins in Devon, UK: a comparative assessment. Sediment budgets: IAHS Publication No. 174: 269-279 (Wallingford).
44. Sadeghi, S.H.R., M. Kiani Harchegani., H.A. Younesi. 2012. Suspended sediment concentration and particle size distribution and their relationship with heavy metals contents. Journal of Earth System Science, 121(1): 63-71. [DOI:10.1007/s12040-012-0143-4]
45. Walling, D.E and J.C. Woodward. 1995. Tracing sources of suspended sediment in river basins: a case study of the River Culm, Devon, UK. Marine and Freshwater Research, 46, 327-336. [DOI:10.1071/MF9950327]
46. Walling, D.E. 2005. Tracing suspended sediment sources in catchments and river systems. Science of the Total Environment, 344: 159-184. [DOI:10.1016/j.scitotenv.2005.02.011]
47. Wood, P.A. 1978. Fine-sediment mineralogy of source rocks and suspended sediment, rother catchment, West Sussex. Earth Surface Processes, 3(3): 255-263. [DOI:10.1002/esp.3290030305]
48. Yamani, M and N. Ebrahimkhani. 2010. Erosion vulnerability assessment through sedimentation alluvium formation of index case study: haji Arab basin (Qazvin province). Geography, 8(24): 69-86.

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