Microscale imaging of phosphate mobility under unsaturated flow as affected by a fertilizer enhancing polymer

Aziz Amoozegar, Dean Hesterberg, Sarah Doydora, Paul Northrup, Samuel Webb
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Abstract

Phosphorus (P) fixation in soil following fertilizer application is a major issue that may be mitigated through a number of methods. Our main objective was to utilize an innovative unsaturated flow system to directly image the mobility of P in soil material as affected by AVAIL, a commercial copolymer phosphate fertilizer enhancer. Air-dried clayey soil material, passed through a 0.25-mm sieve and adjusted to pH 6, was packed in three side-by-side 1.4-cm wide, 20-cm long, and 0.6-cm deep tracks. Water was applied to the tracks under approximately 1 cm tension and moved downstream by sorptivity. Five microliters of aqueous solutions containing 400 mmol P/L and varying levels of AVAIL were applied at a point near the upstream end of each track. Once water passed approximately 6 cm from the point of P application, each track was sectioned into small blocks and air-dried. Synchrotron micro X-ray fluorescence (μ-XRF) images of P, silicon (Si), and aluminum (Al) were collected on block samples to measure relative movement of phosphorus along the soil tracks. Our results show that, despite the high affinity of soil minerals for P, it was relatively mobile with no enhancer under unsaturated flow conditions. Images showed diminished rate of P movement and enhanced clay dispersion with increasing proportion of AVAIL. We postulate that clay dispersion, corroborated by X-ray computed tomography imaging, affected P transport due to interactions with Si and Al minerals. Our results demonstrate the potential utility of our unsaturated flow system combined with μ-XRF imaging to measure convective mobility of plant nutrients or contaminants through soils.

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增肥聚合物对不饱和流动下磷酸盐迁移率影响的微尺度成像
施肥后土壤中磷(P)的固定是一个主要问题,可以通过一些方法来缓解。我们的主要目标是利用一种创新的不饱和流动系统来直接成像受AVAIL(一种商用共聚物磷肥增强剂)影响的土壤材料中P的流动性。风干的粘土材料,通过0.25 mm的筛子,调整到pH值6,在三个并排的1.4 cm宽,20 cm长,0.6 cm深的轨道中包装。在约1cm的张力下,水被施加到轨道上,并通过吸附性向下游移动。5微升的水溶液含有400毫摩尔P/L和不同水平的AVAIL被应用在一个点附近的上游末端每个轨道。一旦水从施磷点约6厘米处流过,每条轨道被切成小块并风干。在块状样品上采集P、硅(Si)和铝(Al)的同步微x射线荧光(μ-XRF)图像,测量磷沿土壤轨迹的相对运动。我们的研究结果表明,尽管土壤矿物质对磷具有很高的亲和力,但在非饱和流动条件下,它是相对流动的,没有增强剂。图像显示,随着AVAIL比例的增加,P的移动速率降低,粘土的分散增强。我们假设粘土分散,通过x射线计算机断层成像证实,由于与Si和Al矿物的相互作用,影响P的运输。我们的研究结果表明,我们的非饱和流动系统结合μ-XRF成像来测量植物养分或污染物通过土壤的对流流动性的潜在效用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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