聚丙烯酸包覆羟基磷灰石纳米颗粒在不饱和水流下在土柱中的迁移

IF 1.9 4区 农林科学 Q3 ENVIRONMENTAL SCIENCES
Zengyu Zhang, Yona Chen, D. Mandler, M. Shenker
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引用次数: 1

摘要

磷(P)纳米颗粒在土壤中比水溶性磷(WSP)具有更大的流动性,因此被建议用作磷肥。不饱和转运是从施用部位到植物根系的主要途径。尽管磷纳米颗粒的不饱和转运对肥效有重要意义,但其定量评价一直被忽视。采用突破柱实验研究了聚丙烯酸(PAA-nHAP)悬浮液和WSP (KH2PO4和K2HPO4的混合物)包覆球形纳米羟基磷灰石颗粒在碱性砂(sandy-alk)、酸性砂质粘土壤土(sandy-ac)和粘性土3种土中非饱和状态下的迁移率。接下来,通过从拆解的土柱中逐层提取总磷来确定磷保留量。在所有土壤中,PAA-nHAP均表现出比WSP更快的迁移速度。在砂石质土壤中,PAA-nHAP的最终相对磷浓度突破较早,但平台较低(分别为输入磷浓度的64.0%和100%),且两种源在10 mM KBr溶液洗涤后的磷保留随深度保持较低。在其他两种土壤中,PAA-nHAP在入口附近表现出较大的滞留,随着深度的增加而减少。在沙质土中,没有WSP, PAA-nHAP最终相对浓度较低(11.6%)。随着深度的增加,PAA-nHAP的保留率远低于WSP。在黏性土壤中,PAA-nHAP比WSP更早突破(P相对浓度>1%)(~35孔体积vs ~45孔体积),洗脱P浓度增加更快(~2.6倍)。两种来源的差异主要发生在土壤表面,土壤表面WSP滞留量较高。土壤性质影响两种磷源的保磷能力,但对所有土壤来说,从普通可溶性肥料改为纳米颗粒肥料增加了磷的流动性。吸附效应和粒径排斥效应是影响nHAP迁移率的主要因素。我们认为可以通过增加负zeta电位修饰其涂层以减少混凝和采用短水力停留时间的滴流来改善nHAP的输运。纳米颗粒的设计需要考虑到土壤的特性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Transport of hydroxyapatite nanoparticles coated with polyacrylic acid under unsaturated water flow in soil columns
ABSTRACT Phosphorus (P) nanoparticles were hypothesized to exhibit greater mobility in soils than water-soluble P (WSP) and were therefore proposed to be used as a P fertilizer. Unsaturated transport is the main pathway from the application site to plant roots. Though its importance to fertilizer efficacy, quantitative evaluation of unsaturated transport of P nanoparticles has been overlooked to date. Mobility of spherical nano-hydroxyapatite particles coated with polyacrylic acid (PAA-nHAP) suspension and WSP (a mixture of KH2PO4 and K2HPO4) was evaluated in breakthrough column experiments under unsaturated states using three soils: alkaline sand (sandy-alk), acidic sandy clay loam (sandy-ac) and clayey soils. Next, P retention was determined by total P extraction layer-by-layer from the disassembled soil columns. In all soils, PAA-nHAP exhibited faster transport compared to WSP. In the sandy-alk soil, earlier breakthrough but lower plateau of the final relative P concentration of PAA-nHAP (64.0% vs. 100% of the input P concentration) and consistent low P retention with depth after washing with 10 mM KBr solution for the two sources were observed. In the other two soils, PAA-nHAP displayed greater retention near the inlet and decreased retention with depth. In the sandy-ac soil, no WSP and low final relative concentrations of PAA-nHAP (11.6%) were transported through the soil column. The retention of PAA-nHAP was much lower than that of WSP with depth. In the clayey soil, the breakthrough (relative P concentration >1%) occurred earlier (~35 pore volumes vs. ~45 pore volumes) and the eluted P concentration increased more rapidly (~2.6 times) for PAA-nHAP compared to WSP. The difference between the two sources mainly occurred at the soil surface with higher retention of WSP. Soil properties affected the P retention capacity of the two P sources, but for all soils, P mobility was increased by changing from the common soluble fertilizers to nanoparticles. Adsorption and size exclusion effect are suggested as the major factors affecting nHAP mobility. We suggest that the nHAP transport can be improved by modifying its coating with more negative zeta-potential to decrease coagulation and adopting drip flows with short hydraulic retention time. The design of the nanoparticles needs to take into account soil properties.
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来源期刊
Soil Science and Plant Nutrition
Soil Science and Plant Nutrition 农林科学-农艺学
CiteScore
4.80
自引率
15.00%
发文量
56
审稿时长
18-36 weeks
期刊介绍: Soil Science and Plant Nutrition is the official English journal of the Japanese Society of Soil Science and Plant Nutrition (JSSSPN), and publishes original research and reviews in soil physics, chemistry and mineralogy; soil biology; plant nutrition; soil genesis, classification and survey; soil fertility; fertilizers and soil amendments; environment; socio cultural soil science. The Journal publishes full length papers, short papers, and reviews.
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