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自发热持续高温好氧堆肥碳、氮、腐殖酸变化过程
引用本文:薛兆骏,彭永臻,王鹏鹞,周国亚,王洪春,贾方旭,景超,王淑莹.自发热持续高温好氧堆肥碳、氮、腐殖酸变化过程[J].中国环境科学,2018,38(11):4094-4098.
作者姓名:薛兆骏  彭永臻  王鹏鹞  周国亚  王洪春  贾方旭  景超  王淑莹
作者单位:1. 北京工业大学国家工程实验室, 北京市水质科学与水环境恢复工程重点实验室, 北京 100124; 2. 鹏鹞环保股份有限公司, 江苏 宜兴 214205
基金项目:国家重点研发计划课题(2016YFC0401102);北京市教委资助项目
摘    要:为了探索超高温自发热好氧污泥堆肥过程中有机碳、氮、腐殖酸变化过程,以1m3小堆体好氧堆肥的形式进行了深入研究.结果表明:水溶性COD从23.18mg/g增大到47.49mg/g,然后逐渐减少至30.67mg/g.总有机碳和TN在前7d减量最多,分别从207.45mg/g,45.40mg/g降到157.86mg/g,38.23mg/g,并在第35d趋于稳定.NH4+-N从9.89mg/g逐渐增加到14.04mg/g,堆肥过程中NO2--N,NO3--N含量极低,总含量低于0.07mg/g,不足TN的0.2%.TN损失达82.87%,主要通过氨气挥发的途径.腐殖酸含量前7d从115.12mg/g迅速上升至214.11mg/g,第21d缓慢下降至154.47mg/g,趋于稳定.腐殖度E4/E6在3.49~4.23范围内变化,总体呈上升趋势,不适用于本工艺腐熟判定.

关 键 词:高温好氧堆肥  有机碳    腐殖酸  
收稿时间:2018-04-25

The transformation regularities of carbon,nitrogen and hunic acid during high temperature aerobic composting process
XUE Zhao-jun,PENG Yong-zhen,WANG Peng-yao,ZHOU Guo-ya,WANG Hong-chun,JIA Fang-xu,JING Chao,WANG Shu-ying.The transformation regularities of carbon,nitrogen and hunic acid during high temperature aerobic composting process[J].China Environmental Science,2018,38(11):4094-4098.
Authors:XUE Zhao-jun  PENG Yong-zhen  WANG Peng-yao  ZHOU Guo-ya  WANG Hong-chun  JIA Fang-xu  JING Chao  WANG Shu-ying
Institution:1. National Engineering Laboratory for Advanced Municipal Wastewater Treatment and Reuse Technology, Key Laboratory of Beijing for Water Quality Science and Water Environment Recovery Engineering, Beijing University of Technology, Beijing 100124, China; 2. Pengyao Environmental Protection Co. Ltd., Yixing 214205, China
Abstract:This paper studied the transformation regularities of key evaluation indicators, such as carbon, nitrogen and humic acid during ultra-high temperature aerobic composting process. The results showed that SCOD increased from 23.18mg/g to 47.49mg/g and then decreased to 30.67mg/g. TOC and TN respectively decreased from 207.45mg/g and 45.40mg/g to 157.86mg/g and 38.23mg/g in the previous seven days and almost remains constant after 35days. In addition, the content of NH4+-N incrased from 9.89mg/g to 14.04mg/g, but the sum of NO2--N and NO3--N (about 0.07mg/g) was less than 2% of TN. The loss of TN was as high as 82.87%, and it mainly attributed to ammonia volatilization. Humic acid increased from 115.12mg/g to 214.11mg/g in previous seven days and alomost remains 154.47mg/g after 21days. Although E4/E6value ranged between 3.49 and 4.23, it showed an increasing trend in total. Hence, it is not suitable for maturity evaluation.
Keywords:ultra-high temperature  organic carbon  nitrogen  humic acid  
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