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تأثیر کاه و کلش گندم بر ویژگیهای جریان و فرسایش شیاری در کشتزار دیم گندم | ||
تحقیقات آب و خاک ایران | ||
مقاله 5، دوره 50، شماره 1، فروردین و اردیبهشت 1398، صفحه 53-63 اصل مقاله (711.37 K) | ||
نوع مقاله: مقاله پژوهشی | ||
شناسه دیجیتال (DOI): 10.22059/ijswr.2018.243817.667774 | ||
نویسندگان | ||
علی رضا واعظی* 1؛ مهدثه حیدری2 | ||
1دانشیار، گروه خاکشناسی، دانشکده کشاورزی، دانشگاه زنجان، زنجان، ایران | ||
2دانشجوی کارشناسی ارشد، گروه خاکشناسی، دانشکده کشاورزی، دانشگاه زنجان، زنجان، ایران | ||
چکیده | ||
فرسایش شیاری یکی از مهمترین علل هدررفت خاک در کشتزارهای دیم شخمخورده در راستای شیب میباشد. افزایش مقدار نفوذ آب به خاک و کاهش نیروی فرسایندگی جریان برای مهار فرسایش شیاری و نیز افزایش عملکرد حائز اهمیت است. این پژوهش با هدف بررسی اثر کاه و کلش گندم بر ویژگیهای هیدرولیکی جریان و فرسایش شیاری در کشتزار دیم گندم در منطقه نیمهخشک در زنجان اجرا شد. آزمایش در قالب طرح بلوک کاملاً تصادفی و با سه تکرار در شرایط مزرعهای با هفت سطح کاه و کلش گندم (صفر، 25، 50، 75، 100، 125 و 150 درصد) و شخم در جهت موازی با شیب انجام شد. در تیمار 100 درصد، مقدار نیم کیلوگرم خاکپوش در هر مترمربع معادل با 5 تن در هکتار مصرف شد. نتایج نشان داد که کاربرد کاه و کلش گندم باعث کاهش معنیدار (05/0>p) سرعت و قدرت جریان و همچنین فرسایش شیاری شد؛ درحالیکه تأثیر آن بر شعاع هیدرولیکی و تنش برشی معنیدار نبود ( 05/0 <p). با افزایش سطح کاه و کلش گندم سرعت و قدرت جریان و همچنین فرسایش شیاری در مقایسه با تیمار شاهد به ترتیب 19، 23 و 55 درصد کاهش یافت. به دلیل پایین بودن عمق جریان آب در شیارهای کشت، مصرف کاه و کلش گندم تأثیری بر شعاع هیدرولیکی و تنش برشی نداشت. همچنین بین فرسایش شیاری و سرعت جریان همبستگی بالا وجود داشت (71/0=r). سطح 100 درصد (پنج تن در هکتار) مصرف کاه و کلش گندم با کاهش 34 و 71 درصدی قدرت جریان و فرسایش شیاری در کشتزار دیم گندم، مناسبترین اثربخشی را از نظر کاهش فرسایش شیاری داشت. در مجموع، کاربرد کاه و کلش گندم راهکاری مناسب و زیستی برای کاهش فرسایندگی جریان و مهار فرسایش شیاری خاک در کشتزارهای دیم میباشد. | ||
کلیدواژهها | ||
افزودنیهای خاک؛ تنش برشی؛ سرعت جریان؛ شعاع هیدرولیکی؛ قدرت جریان | ||
عنوان مقاله [English] | ||
The Effect of Wheat Straw on Flow Characteristics and Rill Erosion in Wheat Rainfed Field | ||
نویسندگان [English] | ||
Ali Reza Vaezi1؛ Mohadeseh Heidari2 | ||
1Associated Professor, Soil Science Department, Faculty of Agriculture University of Zanjan, Zanjan, Iran. | ||
2MSc. Student, Soil Science Department, Faculty of Agriculture University of Zanjan, Zanjan, Iran. | ||
چکیده [English] | ||
Rill erosion is one of the most important reasons of the soil lost in the plowed rainfed fields alongside the slope. Increasing infiltration rate in the soil and decreasing the erosivity of flow is essential for controlling rill erosion as well as increasing crop yield. This research was carried out to find out the effect of wheat straw on hydraulic characteristics of the flow and rill erosion in the wheat rainfed field in semi-arid region in Zanjan. The experiment was performed at seven straw mulch levels (0, 25, 50, 75, 100, 125 and 150 %) using the randomized complete block design with three replicates under the field conditions with plowing alongside the slope. At 100% level, 0.5 kgm-2 equivalent to five tons per hectare of straw mulch was applied into the soil. The results indicated that the effects of wheat straw on flow velocity, flow power and rill erosion was significant (p< 0.05), while its effect on the hydraulic radius and shear stress wasn’t statistically significant. These results were associated with a low depth of flow as affected by straw mulch in the furrow rills (p> 0.05). By increasing the wheat straw mulch level, the flow velocity, flow power and rill erosion decreased about 19, 23 and 55% respectively, as compared to the control treatment. There was a high correlation between the rill erosion and the flow velocity (r=0.71). The 100%-level of wheat straw mulch which decreased the flow power (34%) and the rill erosion (71%), was the most appropriate amount for decreasing rill erosion in rainfed wheat field. Generally, it can be concluded that the application of wheat straw mulch is a biological and proper practice for reducing erosivity of flow and controlling rill erosion in rainfed fields. | ||
کلیدواژهها [English] | ||
Soil amendments, shear stress, Flow velocity, Hydraulic radius, Flow power | ||
مراجع | ||
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