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Stream Water Nitrogen Eutrophication During Non-Irrigated Periods in a Paddy-Dominated Agricultural Basin in a Snowfall Area in Japan

机译:日本降雪地区以稻田为主的农业流域非灌溉期的河流水氮富营养化

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We measured the concentrations of dissolved inorganic nitrogen (DIN; nitrate, ammonium, and nitrite) in stream water in a paddy-dominated agricultural basin in a snowfall area from August 2009 to October 2010 to facilitate evaluation of stream water eutrophication from nitrogen during the non-irrigated period. We compared the nitrogen budget in a paddy field between irrigated and non-irrigated periods, from information about nitrogen fertilizer, denitrification, harvested rice, and atmospheric nitrogen deposition. We also estimated stream nitrogen exports from DIN concentrations and stream flow rates. DIN concentrations in stream water were higher during the non-irrigated period (October-March) than during the irrigated period (April-September). Stream flow was also higher during the non-irrigated period (5.9 mm day(-1)) than during the irrigated period (2.5 mm day(-1)), which possibly reflects snow melting. Although nitrogen fertilizer was applied during the irrigated period, the amount of nitrogen removed by the rice harvest and denitrification was sufficiently large to reduce nitrogen exports from paddy fields. Atmospheric nitrogen deposition was higher during the non-irrigated period (755 kg N km(-2)) than during the irrigated period (410 kg N km(-2)). DIN exports were also higher in the non-irrigated period (860 kg N km(-2)) than in the irrigated period (120 kg N km(-2)). The higher exports in the non-irrigated period may reflect the lack of nitrogen removal by a rice harvest and denitrification and increased runoff and higher atmospheric nitrogen deposition. Our study highlights the important contribution of the non-irrigated period to nitrogen eutrophication in stream water in this particular environment.
机译:我们测量了2009年8月至2010年10月降雪地区以稻田为主的农业流域中溪流水中溶解的无机氮(DIN,硝酸盐,铵和亚硝酸盐)的浓度,以方便评估非干旱期氮对溪流水的富营养化。 -灌溉期。我们根据有关氮肥,反硝化,收获的水稻和大气中氮沉降的信息,比较了灌溉期和非灌溉期稻田的氮素收支。我们还根据DIN浓度和流率估算了流氮的出口。在非灌溉期间(10月至3月),溪流水中的DIN浓度高于灌溉期间(4月至9月)。在非灌溉期间(5.9毫米天(-1)),水流也比灌溉期间(2.5毫米天(-1))高,这可能反映了积雪的融化。尽管在灌溉期间施用了氮肥,但水稻收割和反硝化去除的氮量足够大,可以减少稻田的氮输出。在非灌溉期间(755 kg N km(-2))的大气氮沉积高于在灌溉期间(410 kg N km(-2))。非灌溉期的DIN出口量也较高(860 kg N km(-2)),高于灌溉期(120 kg N km(-2))。非灌溉期的出口量增加可能反映出水稻收割和反硝化不能去除氮,径流增加,大气氮沉降增加。我们的研究强调了在这种特殊环境下,非灌溉期对溪水氮富营养化的重要贡献。

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