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روند تکامل خاک در خاکهای درجا توسعهیافته در یک زمیننمای کوهستان (مطالعه موردی: روستای باندر) | ||
تحقیقات آب و خاک ایران | ||
دوره 53، شماره 1، فروردین 1401، صفحه 141-158 اصل مقاله (2.25 M) | ||
نوع مقاله: مقاله پژوهشی | ||
شناسه دیجیتال (DOI): 10.22059/ijswr.2022.331427.669086 | ||
نویسندگان | ||
مریم اوسط* 1؛ احمد حیدری2 | ||
1استادیار بخش تحقیقات خاک و آب، مرکز تحقیقات و آموزش کشاورزی و منابع طبیعی استان کردستان، سازمان تحقیقات، آموزش و ترویج کشاورزی، | ||
21. استاد، گروه علوم و مهندسی خاک، دانشکده مهندسی و فناوری کشاورزی، پردیس کشاورزی و منابع طبیعی، دانشگاه تهران، کرج، ایران | ||
چکیده | ||
پذیرفتاری مغناطیسی (MS[1]) یکی از شاخصهایی است که در سنجش تکامل خاکرخ مورداستفاده قرار میگیرد. پژوهش حاضر با هدف کارایی پذیرفتاری مغناطیسی در بررسی وضعیت تکامل خاک در یک زمیننمای کوهستانی در منطقه باندر استان مازندران مورد بررسی قرار گرفت. جهت نیل به اهداف مورد بررسی 56 خاکرخ حفر شد و پس از انجام مطالعات صحرایی و آنالیزهای فیزیکوشیمیایی، کلاسهای ردهبندی خاک و شاخص تکامل مورفولوژیک تعیین گردید. برخی از شاخصهای تکامل شیمیایی و ژئوشیمیایی و همچنین پذیرفتاری مغناطیسی در دو فرکانس پایین (χlf) و بالا (χhf) توسط دستگاه Bartington MS2 dual frequency sensor بر روی نمونههای سطحی اندازهگیری شدند. همبستگی بین پذیرفتاری مغناطیسی و کلاسهای ردهبندی خاک، ویژگیهای فیزیکوشیمیایی و شاخصهای تکامل، نشاندهنده کارایی بیشتر پذیرفتاری مغناطیسی و شاخص تکامل مورفولوژیک در نشاندادن وضعیت تکامل خاکهای منطقه میباشد. شیبدار بودن منطقه و همچنین حضور مقادیر بالای کربناتها در منطقه باعث بهوجودآمدن روابط معکوس بین شاخصهای تکامل ژئوشیمیایی و کلاسهای ردهبندی خاک شده است. [1]. Magnetic Susceptibility | ||
کلیدواژهها | ||
پذیرفتاری مغناطیسی؛ شاخص ژئوشیمیایی؛ شاخص مورفولوژیک | ||
مراجع | ||
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