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مروری بر تأثیر اقلیم و تحول خاک بر منابع ذخیره کربن آلی خاک در البرز مرکزی | ||
تحقیقات آب و خاک ایران | ||
دوره 52، شماره 12، اسفند 1400، صفحه 2935-2949 اصل مقاله (1.07 M) | ||
نوع مقاله: مروری | ||
شناسه دیجیتال (DOI): 10.22059/ijswr.2021.330447.669073 | ||
نویسندگان | ||
علیرضا راهب* 1؛ احمد حیدری2 | ||
1استادیار گروه علوم و مهندسی خاک-پردیس کشاورزی و منابع طبیعی دانشگاه تهران | ||
2استاد گروه علوم و مهندسی خاک پردیس کشاورزی و منابع طبیعی دانشگاه تهران | ||
چکیده | ||
تغییرات کربن خاک یکی از مهمترین شاخصهای نشاندهنده تاثیر اقلیم بـر گونههای خـاک اسـت. مدیریت کربن آلی خاک، نیازمند آگاهی از مقدار آن و شناخت عوامل مؤثر بر آن میباشد. در این پژوهش برخی ویژگیهای خاک به ویژه کربن آلی در 76 خاکرخ در اقلیمهای مختلف متشکل از خشک (استان البرز)، نیمهخشک (استان البرز و استان قزوین) و نیمهمرطوب (استان گیلان و مازندران) و مرطوب (استان مازندران) با رژیمهای رطوبتی اریدیک، زریک و یودیک و رژیمهای حرارتی ترمیک و مزیک مورد مطالعه قرار گرفتند. تغییر در پارامترهای اقلیمی سبب ایجاد تغییر تنوع گونهها در اکوسیستم شده و در نهایت بر روی اشکال مختلف کربن به ویژه کربن آلی خاک موثر بوده است. از مهمترین عوامل اقلیمی در این مطالعه میتوان به دما اشاره نمود که افزایش دمای خاک منطقه خشک و نیمهخشک نسبت به دو منطقه مرطوبتر سبب تشدید معدنیشدن شده و در نتیجه آن کربن آلی خاک کاهش مییابد. نتایج نشان داد که مقدار کربن آلی در خاک مناطق مورد مطالعه با افزایش عمق کاهش مییابد و میانگین مقدار کربن آلی در خاکرخهای مالیسول بیشتر از آلفیسولها، اینسپتیسولها، انتیسولها و اریدیسولها بوده است. نتایج کلی این مطالعه نشان میدهد افزایش پارامترهای هدایت الکتریکی خاک (شوری)، اسیدیته خاک و مقدار رس اثر منفی بر میزان کربن آلی خاک، در حالی که افزایش پارامترهای ظرفیت تبادل کاتیونی و مقدار سیلت خاک اثرات مثبت بر آن دارند. | ||
کلیدواژهها | ||
انتیسول؛ کربن آلی؛ اقلیم نیمهخشک؛ تشکیل خاک | ||
عنوان مقاله [English] | ||
A Review of the Effect of Climate and Soil Evolution on Soil Organic Carbon Storage Resources in Central Alborz | ||
نویسندگان [English] | ||
Alireza Raheb1؛ Ahmad Heidari2 | ||
1Assistant Professor -soil science department-College of Agriculture & Natural Resources University of Tehran | ||
2Professor, soil science department, College of Agriculture & Natural Resources,University of Tehran, Karaj, Iran | ||
چکیده [English] | ||
Changes of soil carbon is one of the most important indicators showing the climate impacts on the soil genesis. Soil organic carbon management requires knowledge of its amount and the effective factors. In the current study, the distribution of soil properties especially soil organic carbon were studied in 76 soil profiles consist of different climatic zones arid (Alborz province), semi-arid (Alborz and Qazvin province) and semi-humid (Guilan and Mazandaran province) and humid (Mazandaran province) with aridic, xeric and udic moisture regimes and thermic and mesic temperature regimes. Changes in climatic parameters cause changes in species diversity in the ecosystem and ultimately effect on various forms of carbon, especially soil organic carbon. One of the most important climatic factors in this study is the temperature that increasing the soil temperature in arid and semi-arid regions compared to the two wetter regions causes intensification of mineralization and as a result, soil organic carbon is reduced. The results showed that the amount of organic carbon in the studied soil decreases with increasing depth and the average amount of organic carbon in Mollisols was higher than Alfisols= Inceptisols > Entisols > Aridisols. The general results of this study showed that increasing the parameters of soil electrical conductivity (salinity), soil acidity and clay content have a negative effect, while increasing the parameters of cation exchange capacity and silt content have positive effects on soil organic carbon content. | ||
کلیدواژهها [English] | ||
Entisols, Organic carbon, Semi-arid climate, Soil genesis | ||
مراجع | ||
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