کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4573349 1629471 2014 11 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Flood pulses control soil nitrogen cycling in a dynamic river floodplain
ترجمه فارسی عنوان
پالس های سیل کنترل نیتروژن خاک دوچرخه سواری در یک سیل پویای رودخانه پویا
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فرآیندهای سطح زمین
چکیده انگلیسی


• The effects of flood pulses on nitrogen cycling in floodplain soils were assessed.
• Disturbance by short intensive floods temporarily increased soil N mineralization.
• This further stimulated coupled nitrification–denitrification during soil drying.
• Effects of less intensive floods were much less pronounced.

Flood pulses are major drivers of river–floodplain processes. We investigated their effects on soil nitrogen (N) transformations along a lateral gradient from the river to a mature alluvial forest in the Thur River floodplain (NE Switzerland). Selected N pools (ammonium and nitrate) and N transformations (mineralization, nitrification and denitrification) in the topsoils were repeatedly quantified over a period of six months. During this period, the floodplain was affected by two flood events of different magnitude.Our results showed a distinct difference in size and temporal changes of N pools and transformation rates among functional process zones (FPZs) differing in flooding disturbance. A strong temporary increase in N mineralization in a FPZ with young soil on the frequently flooded gravel bars was the most prominent flood-related effect. This was most likely related to the fast-flowing water during inundation that deposited fresh dispersed sediments with a coarse sandy texture containing highly bioavailable organic N, and/or stimulated the turnover of existing N by destroying sediment aggregates already present before the flood. Increased N mineralization appeared to stimulate coupled nitrification–denitrification in this FPZ during the drying phase. In the more stable FPZs, N mineralization was not strongly enhanced by flooding, whereas nitrification and denitrification were also increased during the drying phase, however to a lesser degree than in the gravel bar soils. Based on our results we propose that floodplain zones characterized by short intensive floods with fast over-flowing water are “hot spots” and the drying phases after the floods are “hot moments” of N transformations.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Geoderma - Volumes 228–229, September 2014, Pages 14–24
نویسندگان
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