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Assessing Seasonal Nitrate Contamination by Nitrate Dual Isotopes in a Monsoon-Controlled Bay with Intensive Human Activities in South China

Author

Listed:
  • Jiacheng Li

    (College of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang 524088, China
    These authors contributed equally to this work.)

  • Ruixue Cao

    (College of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang 524088, China
    These authors contributed equally to this work.)

  • Qibin Lao

    (College of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang 524088, China
    Marine Environmental Monitoring Centre of Beihai, State Oceanic Administration, Beihai 536000, China)

  • Fajin Chen

    (College of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang 524088, China)

  • Chunqing Chen

    (College of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang 524088, China)

  • Xin Zhou

    (College of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang 524088, China)

  • Yafei Meng

    (College of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang 524088, China)

  • Qingmei Zhu

    (College of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang 524088, China)

Abstract

Nitrate (NO 3 − ) dual isotope analysis was performed in Zhanjiang Bay, which is a closed bay with intensive human activities in South China, to investigate seasonal changes in the main NO 3 − sources and their biogeochemical processes in the monsoon-controlled climate. The relatively low N/P ratios in Zhanjiang Bay suggests that nitrogen (N) is a limiting nutrient, which indicates that the increase of N is favorable for phytoplankton proliferation. However, a sufficient amount of ammonium was found in our study area owing to intensive human activities, which can support biological processes. Thus, less NO 3 − biological processes were found, indicating that NO 3 − isotopic characteristics may reveal details of the mixing from various sources. The Bayesian mixing model showed that NO 3 − in the upper bay originated from manure (43%), soil N (30%), N fertilizer (17%), and N precipitation (10%) during winter, which reflects the local human activities; while NO 3 - sources during summer were mainly N fertilizer (36%), soil N (32%), and manure (31%), indicating the source as the runoff from the upper river basin. Our results suggest that nitrate dual-isotope was very useful for tracing the main NO 3 − sources in the condition of the sufficient ammonium, and runoff exerted an important impact on the shift in NO 3 − sources between both the local source and the source from the upper river basin during the two seasons in this monsoon-controlled bay.

Suggested Citation

  • Jiacheng Li & Ruixue Cao & Qibin Lao & Fajin Chen & Chunqing Chen & Xin Zhou & Yafei Meng & Qingmei Zhu, 2020. "Assessing Seasonal Nitrate Contamination by Nitrate Dual Isotopes in a Monsoon-Controlled Bay with Intensive Human Activities in South China," IJERPH, MDPI, vol. 17(6), pages 1-16, March.
  • Handle: RePEc:gam:jijerp:v:17:y:2020:i:6:p:1921-:d:332889
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    Cited by:

    1. Jiang, Weilong & Yang, Fang & Wang, Xihuan & Miao, Qingfeng & Ji, Meicheng & Pan, Ting & Wang, Qianqian & Han, Zhiming & Feng, Weiying & Liao, Haiqing, 2024. "Improved determination of nitrate isotopes in irrigated agricultural areas and Bayesian mixing model quantification of nitrate sources and fate," Agricultural Water Management, Elsevier, vol. 298(C).

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