Effects of Some local Conditions on Leaching Factor of Aridisols in Kalar/Garmian, Kurdistan- Iraq

Five sites were selected in Kalar city on different topographic position. The mean annual rainfall of the study area about 280 mm with about 24.5 C° mean annual temperature. The study area used for rain feed crop production. Morphological properties of the studied pedons indicated that all pedons we...

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Main Author: Salim Neimat Azeez
Format: Article
Language:English
Published: Sulaimani Polytechnic University 2016-12-01
Series:Kurdistan Journal of Applied Research
Subjects:
Online Access:http://kjar.spu.edu.iq/index.php/kjar/article/view/18
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spelling doaj-a7d45502e7fd48b79201a2de039c0b862020-11-25T00:20:24ZengSulaimani Polytechnic UniversityKurdistan Journal of Applied Research2411-76842411-77062016-12-0112202510.24017/science.2016.1.2.118Effects of Some local Conditions on Leaching Factor of Aridisols in Kalar/Garmian, Kurdistan- IraqSalim Neimat Azeez0Sulaimani Polytechnic University, Darbandikhan Technical Institute Darbandikhan, Sulaimani, Kurdistan Region, IraqFive sites were selected in Kalar city on different topographic position. The mean annual rainfall of the study area about 280 mm with about 24.5 C° mean annual temperature. The study area used for rain feed crop production. Morphological properties of the studied pedons indicated that all pedons were developed with Ochric epipedons and Cambic and Argillic endopedons .The results of particle size distribution show a wide differences between sand and clay in surface horizons except pedon (2) because of low elevation compared with other pedons. Moreover, the results of exchangeable sodium and potassium indicate that pedons (4) and (5) had the lowest value of soil leaching factor which is an indication of the high activity of weathering and leaching processes. In another hand, the results of total element analysis has observed that the silicate ratio were high to indicate the high leaching processes which is the proof of the existence of fine materials movement particularly clay colloids, this is not merely due to the rare rainy weather conditions that are prevalent recently but is a result of wet paleoclimatic conditions, and this movement eventually occurred due to in situ factors. All soils are belonged to Aridisols order with suborders Argids and Cambidsas these soils are in aridic moisture regime include Ochric diagnostic surface horizon with Argillic and Cambic diagnostic subsurface horizons.http://kjar.spu.edu.iq/index.php/kjar/article/view/18Soil leaching factor, Aridisols, Epipedon, Endopedon
collection DOAJ
language English
format Article
sources DOAJ
author Salim Neimat Azeez
spellingShingle Salim Neimat Azeez
Effects of Some local Conditions on Leaching Factor of Aridisols in Kalar/Garmian, Kurdistan- Iraq
Kurdistan Journal of Applied Research
Soil leaching factor, Aridisols, Epipedon, Endopedon
author_facet Salim Neimat Azeez
author_sort Salim Neimat Azeez
title Effects of Some local Conditions on Leaching Factor of Aridisols in Kalar/Garmian, Kurdistan- Iraq
title_short Effects of Some local Conditions on Leaching Factor of Aridisols in Kalar/Garmian, Kurdistan- Iraq
title_full Effects of Some local Conditions on Leaching Factor of Aridisols in Kalar/Garmian, Kurdistan- Iraq
title_fullStr Effects of Some local Conditions on Leaching Factor of Aridisols in Kalar/Garmian, Kurdistan- Iraq
title_full_unstemmed Effects of Some local Conditions on Leaching Factor of Aridisols in Kalar/Garmian, Kurdistan- Iraq
title_sort effects of some local conditions on leaching factor of aridisols in kalar/garmian, kurdistan- iraq
publisher Sulaimani Polytechnic University
series Kurdistan Journal of Applied Research
issn 2411-7684
2411-7706
publishDate 2016-12-01
description Five sites were selected in Kalar city on different topographic position. The mean annual rainfall of the study area about 280 mm with about 24.5 C° mean annual temperature. The study area used for rain feed crop production. Morphological properties of the studied pedons indicated that all pedons were developed with Ochric epipedons and Cambic and Argillic endopedons .The results of particle size distribution show a wide differences between sand and clay in surface horizons except pedon (2) because of low elevation compared with other pedons. Moreover, the results of exchangeable sodium and potassium indicate that pedons (4) and (5) had the lowest value of soil leaching factor which is an indication of the high activity of weathering and leaching processes. In another hand, the results of total element analysis has observed that the silicate ratio were high to indicate the high leaching processes which is the proof of the existence of fine materials movement particularly clay colloids, this is not merely due to the rare rainy weather conditions that are prevalent recently but is a result of wet paleoclimatic conditions, and this movement eventually occurred due to in situ factors. All soils are belonged to Aridisols order with suborders Argids and Cambidsas these soils are in aridic moisture regime include Ochric diagnostic surface horizon with Argillic and Cambic diagnostic subsurface horizons.
topic Soil leaching factor, Aridisols, Epipedon, Endopedon
url http://kjar.spu.edu.iq/index.php/kjar/article/view/18
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