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Fate and distribution of nutrients and heavy metals during hydrothermal carbonization of sewage sludge with implication to land application

机译:污泥水热碳化过程中养分和重金属的赋存与分布及其对土地利用的影响

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摘要

Hydrothermal carbonization has been considered effective to reduce sewage sludge volume and provide an opportunity to generate valuable byproducts for a wide range of potential applications. The fate and distribution of nutrients during hydrothermal carbonization of sewage sludge, along with that of heavy metals, is very important for realizing nutrient recovery and reuse by both hydrochar and liquid phase directly as soil amendments and/or organic fertilizer. In this study, we systematically investigated the migration and transformation of nutrients and heavy metals using chemical extractions and reaction severity (Ruyter model) methods at a temperature range of 120-300 degrees C for 30-180 min. With increasing reaction severity, carbon and nitrogen efficiency of hydrochar showed a liner and exponential decrease respectively, while phosphorus accumulated positively in hydrochar. Nitrogen species in hydrochar are mostly nitrogen-containing aromatic heterocycles whereas in liquid phase are predominantly ammonia N and organic-N. The organic phosphorus in sewage sludge was transformed to inorganic species but non-apatite phosphorus showed an exponential reduction in hydrochar with increasing reaction severity, together with the decrease of orthophosphate in liquid phase. As for heavy metals, hydro thermal carbonization promoted decrease in direct bioavailable fractions (except arsenic) and increase in stable fraction (except cadmium and arsenic) in hydrochar as reaction severity elevated. Since hydro thermal effects led to redistribution of nutrients speciation and immobilization of heavy metals, non-farm land application of both hydrochar and liquid phase seems to be possible and unrestricted. This study provides fundamental knowledges for the construction of sludge management strategies to better nutrients recycling and reclamation. (C) 2019 Elsevier Ltd. All rights reserved.
机译:水热碳化被认为有效地减少了污水污泥的量,并提供了产生有价值的副产物的机会,可用于广泛的潜在应用。污水污泥热碳碳化过程中养分的命运和分布以及重金属的分布对于直接利用碳氢化合物和液相作为土壤改良剂和/或有机肥料实现养分的回收和再利用非常重要。在这项研究中,我们使用化学提取和反应强度(Ruyter模型)方法在120-300摄氏度的温度范围内30-180分钟系统地研究了营养物和重金属的迁移和转化。随着反应强度的增加,碳氢化合物的碳和氮效率分别呈线性下降和指数下降,而磷在碳氢化合物中正积累。水碳中的氮种类主要是含氮芳族杂环,而液相中的氮主要是氨氮和有机氮。污水污泥中的有机磷转化为无机物,但非磷灰石的磷随着反应严重程度的增加,其碳氢化合物呈指数下降,液相中的正磷酸盐呈下降趋势。对于重金属,随着反应严重程度的提高,水热碳化促进了水焦中直接生物利用馏分(砷除外)的减少和稳定分数(镉和砷除外)的增加。由于水热效应导致养分形态的重新分布和重金属的固定化,因此非农田土地上既可以使用水焦油,也可以使用液相,这似乎是可能的,而且不受限制。这项研究为构建污泥管理策略提供了基础知识,以更好地进行养分循环利用。 (C)2019 Elsevier Ltd.保留所有权利。

著录项

  • 来源
    《Journal of Cleaner Production》 |2019年第10期|972-983|共12页
  • 作者单位

    Inner Mongolia Univ, Sch Ecol & Environm, Minist Educ, Key Lab Ecol & Resource Use Mongolian Plateau, Hohhot 010021, Inner Mongolia, Peoples R China|Inner Mongolia Univ, Inner Mongolia Key Lab Coal Chem Ind Wastewater T, Hohhot 010021, Inner Mongolia, Peoples R China;

    Jining Environm Protect Bur, Environm Monitoring Ctr, Ulanqab 012000, Inner Mongolia, Peoples R China;

    Inner Mongolia Univ, Sch Ecol & Environm, Minist Educ, Key Lab Ecol & Resource Use Mongolian Plateau, Hohhot 010021, Inner Mongolia, Peoples R China|Inner Mongolia Univ, Inner Mongolia Key Lab Coal Chem Ind Wastewater T, Hohhot 010021, Inner Mongolia, Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Hydrochar; Liquid phase; Reaction severity; Chemical speciation; Migration and transformation;

    机译:水焦;液相;反应强度;化学形态;迁移转化;

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