the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Enhanced isotopic approach combined with microbiological analyses for more precise distinction of various N-transformation processes in contaminated aquifer – a groundwater incubation study
Abstract. This study explores nitrogen transformations in groundwater from an agricultural area utilizing organic fertilizer (wastewaters from yeast production) integrating isotopic analysis, microbial gene abundance, and the FRAME (isotope FRactionation And Mixing Evaluation) model to trace and quantify nitrogen cycling pathways. Groundwater samples with elevated nitrate concentrations were subjected to controlled laboratory incubations with application of a novel low-level 15N tracing strategy, to investigate microbial processes. Isotope analyses of nitrate, nitrite and nitrous oxide (N2O), coupled with microbial gene quantification via quantitative PCR (qPCR), revealed a shift from archaeal-driven nitrification to bacterial denitrification in post-incubation suboxic conditions, stimulated by glucose addition. FRAME modeling further identified bacterial denitrification (bD) as the dominant pathway of N2O production, which was supported by increased nosZI, nirK and nirS gene abundance and observed isotope effects.
Simultaneously to the intensive nitrate reduction, it was observed that the majority of nitrite is likely produced through nitrification processes linked to dissolved organic nitrogen (DON) oxidation. Nitrate reduction had minor contribution in the total nitrite pool. The results demonstrate the efficacy of integrating multi-compound isotope studies and microbial analyses to unravel nitrogen cycling mechanisms. This approach provides a robust framework for addressing nitrogen pollution in groundwater systems and improving water quality management strategies.
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Status: open (until 26 Apr 2025)
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RC1: 'Comment on egusphere-2025-754', Anonymous Referee #1, 27 Mar 2025
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Major Comments
One of the highlights of the manuscript “Enhanced isotopic approach combined with microbiological analyses for more precise distinction of various N-transformation processes in contaminated aquifer – a groundwater incubation study” is the simultaneous use of isotopic labeling and natural abundance stable isotope methods to investigate the nitrogen cycling processes in groundwater and the sources of nitrous oxide (N₂O) production. The study found that nitrite (NO2-) may originate from the mineralization of dissolved organic nitrogen (DON) under conditions of high dissolved organic nitrogen. Furthermore, the nitrogen transformation processes are highly sensitive to the availability of organic carbon. The increase in the C/N ratio due to the additional organic carbon promotes the transition of nitrification processes to denitrification processes in groundwater. This manuscript is significant for a deeper understanding of the sources of nitrogen pollution in groundwater and the migration and transformation processes of nitrogen. The conclusions of this study provide theoretical support for explaining the sources and mechanisms of high nitrate pollution in groundwater.
Specific comments
- Line 45-48: It is suggested to explain the specific anthropogenic sources and natural processes involved in groundwater.
- Line 138-139: Supplement the salinity and dissolved oxygen concentration values of the groundwater samples collected from the monitoring wells.
- Line 139-142: Why were these four monitoring well water samples selected for laboratory cultivation? Please clarify the selection criteria.
- Line 181-188: Indicate the detection limits for the inorganic nitrogen analysis methods.
- Line 204-207: What is the spatial relationship between these monitoring wells and the discharge point (the retention area for yeast production wastewater)? Is there a possibility that the high DON in the yeast wastewater mineralizes to ammonium and subsequently nitrifies to NO3-? Table 1 shows that the monitoring wells with high NO3- concentrations also have higher DON concentrations (except for the discharge point P-L1). If this is the case, it is necessary to also focus on monitoring wells with high ammonium and low NO3- to compare with high NO3- water samples, thus revealing the process of high DON converting to NO3- in groundwater and the nitrogen transformation conditions.
- Line 213-215: Does this mean that the DO concentration in the water of the monitoring wells falls within this range? Since this data is not shown in Table 2, it is suggested to include the DO concentration values of the field monitoring wells in Table 1.
- Line 220-221: Why is the volume of the added labeled liquid different here?
- Line 263-266: Please specify the detection limit for the denitrifying bacteria method.
- Line 308-309: The NO3- concentration in the P-0 monitoring well is higher than that in P-7, yet it was not selected for further cultivation studies. Why?
- Line 314-316: Please add the detection method for NH4+ isotopes and its detection limit in the methods section.
- 第 600 行:应该“标记为 NO3- 还原”吗?
- 第 632-633 行:根据图 7,在添加葡萄糖之前,一些点(尽管它们的 NO2- 浓度较低)倾向于异养硝化,而在添加后,它们更多地聚集在自养硝化范围内。请验证数据并更正结果描述。
- 第 804-806 行:这个结论非常有趣。在培养期间是否同时监测了 DON?DON 变化的幅度是多少?
- 第 845-846 行:本研究中收集的样品均含有高 NO3- 或 DON,NH4+ 浓度高的样品未进行分析。因此,高铵态条件下 NO2- 的来源以及当时 NO2- 和 DON 之间的关系无法显示。这是该研究的一个重大局限性。建议在讨论中解决这个问题。
Citation: https://doi.org/10.5194/egusphere-2025-754-RC1
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