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Information Journal Paper

Title

AN INVESTIGATION OF THE EFFECT OF SOURCE AREA LITHOLOGY ON INFILTRATION RATES OF ALLUVIAL DEPOSITS

Pages

  289-299

Abstract

 Physical and chemical properties of sediments are affected by source area LITHOLOGICAL FORMATIONs. If these deposit materials exist in flood spreading systems or artificialrecharge basins the INFILTRATION RATE will be decreased. Therefore, the rate of infiltration in alluvial deposits is indirectly related to source area lithology. Suitable areas for determining these relationships were selected. In this research, 8 small watersheds with relatively uniform lithology at UPSTREAM of BAND-SARs (Traditional Flood Harvesting Systems) were selected in 20 million hectares in KHORASAN PROVINCE. INFILTRATION RATEs in BAND-SARs as well as in control areas were determined. The results show that the INFILTRATION RATE in the 8 regions are completely different and related to UPSTREAM LITHOLOGICAL FORMATION. Coarse grained sedimentary and igneous formations have little effect on the decrease in INFILTRATION RATE.

Cites

References

Cite

APA: Copy

KAMALI, K., ARAB KHEDRI, M., ESFANDIARI, M., & ZARIN KAFSH, M.. (2005). AN INVESTIGATION OF THE EFFECT OF SOURCE AREA LITHOLOGY ON INFILTRATION RATES OF ALLUVIAL DEPOSITS. IRANIAN JOURNAL OF NATURAL RESOURCES, 58(2), 289-299. SID. https://sid.ir/paper/22739/en

Vancouver: Copy

KAMALI K., ARAB KHEDRI M., ESFANDIARI M., ZARIN KAFSH M.. AN INVESTIGATION OF THE EFFECT OF SOURCE AREA LITHOLOGY ON INFILTRATION RATES OF ALLUVIAL DEPOSITS. IRANIAN JOURNAL OF NATURAL RESOURCES[Internet]. 2005;58(2):289-299. Available from: https://sid.ir/paper/22739/en

IEEE: Copy

K. KAMALI, M. ARAB KHEDRI, M. ESFANDIARI, and M. ZARIN KAFSH, “AN INVESTIGATION OF THE EFFECT OF SOURCE AREA LITHOLOGY ON INFILTRATION RATES OF ALLUVIAL DEPOSITS,” IRANIAN JOURNAL OF NATURAL RESOURCES, vol. 58, no. 2, pp. 289–299, 2005, [Online]. Available: https://sid.ir/paper/22739/en

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