Back to Search Start Over

The dynamic features and microbial mechanism of nitrogen transformation for hydrothermal aqueous phase as fertilizer in dryland soil.

Authors :
Huang, Hua
He, Maoyuan
Liu, Xiaoyan
Ma, Xiaoli
Yang, Ying
Shen, Yuanlei
Yang, Yujia
Zhen, Yanzhong
Wang, Jian
Zhang, Yongtao
Wang, Shuai
Shan, Xianying
Fan, Wenyan
Guo, Di
Niu, Zhirui
Source :
Journal of Environmental Management. Apr2024, Vol. 356, pN.PAG-N.PAG. 1p.
Publication Year :
2024

Abstract

Hydrothermal aqueous phase (HAP) contains abundant organics and nutrients, which have potential to partially replace chemical fertilizers for enhancing plant growth and soil quality. However, the underlying reasons for low available nitrogen (N) and high N loss in dryland soil remain unclear. A cultivation experiment was conducted using HAP or urea to supply 160 mg N kg−1 in dryland soil. The dynamic changes of soil organic matters (SOMs), pH, N forms, and N cycling genes were investigated. Results showed that SOMs from HAP stimulated urease activity and ureC , which enhanced ammonification in turn. The high-molecular-weight SOMs relatively increased during 5–30 d and then biodegraded during 30–90 d, which SUV 254 changed from 0.51 to 1.47 to 0.29 L−1 m−1. This affected ureC that changed from 5.58 to 5.34 to 5.75 lg copies g−1. Relative to urea, addition HAP enhanced ON mineralization by 8.40 times during 30–90 d due to higher ureC. It decreased NO 3 –N by 65.35%–77.32% but increased AOB and AOA by 0.25 and 0.90 lg copies g−1 at 5 d and 90 d, respectively. It little affected nirK and increased nosZ by 0.41 lg copies g−1 at 90 d. It increased N loss by 4.59 times. The soil pH for HAP was higher than that for urea after 11 d. The comprehensive effects of high SOMs and pH, including ammonification enhancement and nitrification activity inhibition, were the primary causes of high N loss. The core idea for developing high-efficiency HAP fertilizer is to moderately inhibit ammonification and promote nitrification. [Display omitted] • HAP relative to urea increased N loss by 4.59 times during 90 d cultivation. • HAP increased ureC during 30–90 d when high molecular weight DOMs biodegraded. • HAP increased AOA + AOB by 0.95 lg copies g−1 but decreased 65.35%–77.32% NO 3 –N. • HAP little changed nirK and increased nosZ by 0.41 lg copies g−1. • High soil pH and SOMs reasoned from HAP were the main reasons. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
03014797
Volume :
356
Database :
Academic Search Index
Journal :
Journal of Environmental Management
Publication Type :
Academic Journal
Accession number :
176391530
Full Text :
https://doi.org/10.1016/j.jenvman.2024.120643