伊尔加兹山脉冰缘地貌发育和土壤形成及其气候的影响(土耳其黑海西岸)
Development of periglacial landforms and soil formation in the Ilgaz Mountains and effect of climate(Western Black Sea Region-Türkiye)作者机构:Department of GeographyArdahan UniversityArdahan75002Türkiye Department of Soil Science and Plant NutritionFaculty of AgricultureOndokuz Mayıs UniversitySamsun55139Türkiye Department of GeographyFaculty of Human and Social SciencesSamsun UniversitySamsun55080Türkiye Center for Climate Change and Policy StudiesBoğaziçi Universityİstanbul34342Türkiye Faculty of AgricultureDepartment of Soil Science and Plant NutritionIsparta University of Applied SciencesIsparta32200Türkiye Institute of Social Sciencesİstanbul Universityİstanbul34119Türkiye
出 版 物:《Journal of Geographical Sciences》 (地理学报(英文版))
年 卷 期:2024年第34卷第3期
页 面:543-570页
核心收录:
学科分类:07[理学] 070601[理学-气象学] 0706[理学-大气科学]
基 金:Scientific Research Projects Coordinatorship which supported the study with the project
主 题:periglacial landforms soil formation climate effect Ilgaz Mountains Türkiye
摘 要:The main aims of the current study are to determine the morphological features of the periglacial landforms(non-sorted step,mud circle,stony earth circle,thufur,and congeliturbation)located on the Ilgaz Mountains,examine the physicochemical and mineralogical properties with pedological processes of the soils,and assess of the effects of climatic conditions controlling the development of *** Ilgaz Mountains(2587 m a.s.l.),located in the Western Black Sea Region,within the Anatolian Mountains,are important in terms of periglacial landforms(mud circles,stony earth circles,thufurs,non-sorted steps,non-sorted stripes,congeliturbation deposits,and block currents).The descriptive statistics of 123 periglacial landforms measured by fieldworks were *** distribution of freezing and thawing in the Ilgaz Mountains throughout the year was evaluated,and it was found that freezing takes place between December and March,freezing-thawing takes place in April,May,October and November,and thawing takes place between June and *** to soil properties,organic matter content changes from 1.88%to 12.72%in non-sorted step soils,while it is between 2.03%and 12.24%in stony earth circle *** organic matter is observed to be close to congeliturbation deposits at lower ratios compared to non-sorted steps,stony earth circles and mud *** soil reactions on stony earth circles and non-sorted steps vary between slightly acidic and slightly *** the other hand,soil samples taken from the mud circles are different from those taken from the non-sorted steps and stony earth *** soil reaction is acidic,and pH changes between 4.86 and *** lime content also varies between 2.81%and 32.08%,with an average of 12.02%.The texture properties of soils are dominantly loam and clay loam,as in the non-sorted steps,stony earth circles,and mud *** their mineralogical properties,the XRD study was carried out to determine the primer mineral