کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4478321 1622913 2016 8 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Loss of soil phosphorus by tile drains during storm events
ترجمه فارسی عنوان
از دست دادن فسفر خاک توسط تخلیه کاشی در حوادث طوفان
کلمات کلیدی
اشباع فسفر؛ نقشه برداری عنصر؛ حفاظت از آب های سطحی؛ کیفیت آب
موضوعات مرتبط
علوم زیستی و بیوفناوری علوم کشاورزی و بیولوژیک علوم زراعت و اصلاح نباتات
چکیده انگلیسی


• Storm event in summer resulted in loss of P rich ochre flocs from tile drains.
• Floating fungal mycelia were identified as carrier for Fe and P.
• Flocky nature of ochre suggested high temporal bioavailability of P in water.
• Retention of P at drain outlet is recommended.

Phosphorus losses from agricultural soils are usually predominately caused by surface-runoff and only rarely by tile drain discharge. However, storm events can drastically increase P transfer to water bodies. In 2011 summer storm events caused 3.2 fold higher precipitation compared to the long-term average in Northern Germany. During these storm events excessive yellow-brown ochre flocs were observed in drain discharges and supposed to be potential P carrier. Therefore, water samples with ochre flocs were taken and analyzed by light and electron microscopy and for total elemental concentrations of P and its common binding partners (Al, Fe, Mn). Additionally, sandy sediment samples were taken in winter and analyzed for total and oxalate-extractable amounts of these elements. Water samples with ochre flocs revealed total P concentrations of approximately 27 to 141 mg l−1. During the high discharge period a cumulative discharge of 124.6 mm from a drain plot of 4.2 ha was recorded, which resulted in a calculated minimum loss of 34 kg Pt ha−1. This was assumed to be promoted by the excessive occurrence of ochre flocs, which were mainly formed by fungal mycelia with precipitated Fe- and Mn-(hydr)oxides at the surface. The poor crystallinity of the Fe-oxides from the discharge of tile drains was confirmed by an amount of up to 94% of active Fe-oxides in the sandy sediment. The extremely high discharge from tile drains, the flocky nature of the ochre along with a poor crystallinity of Fe-oxides and high P concentrations possess the risk of increased input and bioavailability of P in water bodies. Therefore, discharge and P forms from tile drained areas should be monitored more intensively and retention of P on tile drain outlets should be considered to prevent water bodies from eutrophication.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Agricultural Water Management - Volume 167, 31 March 2016, Pages 21–28
نویسندگان
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