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اثر شوری خاک بر معدنی شدن نیتروژن در حضور و عدم حضور کلش گندم در سه خاک با کلاس بافتی متفاوت | ||
تحقیقات آب و خاک ایران | ||
دوره 54، شماره 12، اسفند 1402، صفحه 1913-1928 اصل مقاله (1.62 M) | ||
نوع مقاله: مقاله پژوهشی | ||
شناسه دیجیتال (DOI): 10.22059/ijswr.2023.366817.669589 | ||
نویسندگان | ||
یونس شکوهی فر1؛ احمد محمدی قهساره* 2؛ کریم شهبازی3؛ محمدمهدی طهرانی*4؛ حسین بشارتی5 | ||
1دانشجوی دکترای شیمی و حاصلخیزی خاک، گروه خاکشناسی، دانشکده کشاورزی و منابع طبیعی، واحد اصفهان (خوراسگان)، دانشگاه آزاد اسلامی، | ||
2گروه خاکشناسی، دانشکده کشاورزی و منابع طبیعی، واحد اصفهان (خوراسگان)، دانشگاه آزاد اسلامی، اصفهان، ایران. | ||
3بخش آزمایشگاه ها، موسسه تحقیقات خاک و آب، سازمان تحقیقات، آموزش و ترویج کشاورزی، کرج، ایران | ||
4بخش تحقیقات حاصلخیزی خاک و تغذیه گیاه، موسسه تحقیقات خاک و آب، سازمان تحقیقات، آموزش و ترویج کشاورزی، کرج، ایران | ||
5بخش تحقیقات بیولوژی خاک، موسسه تحقیقات خاک و آب، سازمان تحقیقات، آموزش و ترویج کشاورزی،کرج، ایران | ||
چکیده | ||
این مطالعه بهمنظور بررسی اثر شوری خاک بر معدنی شدن نیتروژن در حضور و عدم حضور کلش گندم درسه خاک با کلاس بافتی رسی، لومی و شنی لومی در شرایط آزمایشگاهی بصورت فاکتوریل در قالب طرح کاملاً تصادفی با فاکتورهای شوری (1، 10، 20 و 30 دسیزیمنس بر متر)، کلش گندم (صفر و 2 درصد وزنی با 5/89=C/N) و زمان (روزهای 2، 5، 12، 20، 28، 37، 46، 53، 64، 73، 85 و90) در 3 تکرار اجرا شد. نمونه خاکهای زراعی مناطق مختلف ایران بررسی و سه خاک با شوری پایین (1/1-84/0 دسیزیمنس بر متر) و کربن آلی کم (98/0-22/0 درصد) انتخاب شدند. آزمایش نتایج بدست آمده نشان داد که در هر سه نوع خاک غلظت آمونیوم و نیترات در تیمار بدون کلش بیشتر از تیمار دارای کلش بود. در تیمار دارای کلش یک روند کاهشی اولیه در مقدار آمونیوم و نیترات برای هر سه خاک وجود داشت ولی پس از مدت زمانی، مقدار آمونیوم و نیترات خاک روند افزایشی و بازگشت به مقدار اولیه را نشان داد. با افزایش سطح شوری خاک، مقدار آمونیوم خاک در خاکهای رسی و شن لومی، افزایش یافت در حالیکه در خاک لوم کاهش یافت. مقدار نیترات در هر سه نوع خاک با افزایش سطح شوری، روند کاهشی نشان داد. بطورکلی یافتههای این تحقیق نشان داد که حضور کلش در خاک میتواند اثرات منفی غلظتهای بالای نمک را بر معدنی شدن نیتروژن تعدیل کرده و از تلفات آن بکاهد. | ||
کلیدواژهها | ||
آمونیوم؛ تلفات نیتروژن؛ ماده آلی؛ نیترات؛ قابلیت هدایت الکتریکی | ||
عنوان مقاله [English] | ||
The effect of soil salinity on nitrogen mineralization in the presence and absence of wheat straw in three soils with different textural classes | ||
نویسندگان [English] | ||
Younes Shukuhifar1؛ Ahmad Mohammadi Ghehsareh2؛ Karim Shahbazi3؛ Mohammad mehdi Tehrani4؛ Hosein Besharati5 | ||
1PhD student of Soil Science, Department of Soil Science, Faculty of Agriculture and Natural Resources, Isfahan (Khorasgan) Branch, Islamic Azad University, Isfahan, Iran | ||
2Department of Soil Science, Faculty of Agriculture and Natural Resources, Isfahan (Khorasgan) Branch, Islamic Azad University, Isfahan, Iran | ||
3Department of Laboratories,, Soil and Water Research Institute, Agricultural Research Education and Extension Organization, Karaj, Iran | ||
4Department of Soil Fertility and Plant Nutrition,, Soil and water research institute, Agricultural Research Education and Extension Organization, Karaj, Iran | ||
5Department of Soil Biology, Soil and Water Research Institute, Agricultural Research Education and Extension Organization, Karaj, Iran | ||
چکیده [English] | ||
This study was conducted to investigate the effect of soil salinity on nitrogen mineralization in the presence and absence of wheat straw in three soils with textural classes of clay, loam and loamy sand under laboratory conditions as a factorial arrangement based on a completely randomized design with 3 replications. The studied factors were salinity (1, 10, 20 and 30 dS/m), wheat straw (0 and 2% by weight with C/N=89.5) and time (2, 5, 12, 20, 28, 37, 46, 53, 64, 73, 85 and 90 days). After investigation of different Iranian agricultural soils, three soils with low salinity (0.84-1.1 dS/m) and low organic carbon (0.22-0.98%) were selected. Considering the results, in the three soils, the amount of ammonium and nitrate in the treatment without straw was higher than those in the treatment with straw. In straw treatment, there was an initial descending trend in the amount of ammonium and nitrate for the three soils, but after a period of time, ammonium and nitrate content of the soil showed an ascending trend and returned to the initial value. With increasing soil salinity, the amount of soil ammonium increased in clay and loamy sand soils but decreased in the loamy soil. Nitrate content showed a descending trend for the three soils with increasing salinity. In general it is concluded that the presence of wheat straw in the soil can mitigate the negative effects of high concentrations of salt on nitrogen mineralization and reduce nitrogen losses. | ||
کلیدواژهها [English] | ||
Ammonium, Electrical conductivity, Nitrate, Nitrogen losses, Organic matter | ||
مراجع | ||
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