Variation of deep nitrate in a typical red soil Critical Zone: Effects of land use and slope position

Shun-Hua Yang, Hua-Yong Wu* (Corresponding Author), Xiao-Dong Song, Yue Dong, Xiao-Rui Zhao, Qi Cao, Jin-Ling Yang, Gan-Lin Zhang* (Corresponding Author)

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

24 Citations (Scopus)

Abstract

There is evidence that high levels of nitrate are stored in Earth's Critical Zone between the land surface and impermeable bedrock. While nitrate in the upper layers of the soil (<1 m) has been extensively studied, less information is available on its variation and the controlling factors at depth (> 1 m). To study controls on nitrate accumulation in a subtropical monsoon area, a total of 728 regolith samples, taken from land surface to fresh bedrock, were collected from 21 drillings in a typical red soil Critical Zone in southern China. We characterized the variation of nitrate in these deep horizons and investigated the effect of land use, slope position and regolith physiochemical properties. The results showed that the amount of nitrate at 240-380 cm depth was more stable than at 100-240 cm or 380-500 cm depth, and accumulated at that depth in the upland and orchard regoliths. Nitrate contents in the deep horizons of upland and orchard regoliths were significantly larger than that in the paddy fields or woodland (p <0.05). When compared to the regoliths from the upper slope of the upland, those from the middle slope stored significantly more nitrate in the deep regolith layer (p <0.05). Soil pH was the most important single variable in explaining nitrate variability, followed by particle-size distribution (sand, silt and clay) at the point scale. We found that land-use was the most important control in explaining nitrate variation followed by slope position and finally regolith physiochemical properties. These results suggest that deep regoliths of the uplands and orchards in humid regions are most likely to hold a large reservoir of nitrate, which has routinely been overlooked in the past. Moreover, the dominant physiochemical properties of the regolith in controlling the nitrate levels varied among different layers. The findings could have significant implications for biogeochemical cycling of nitrogen in deep soil layers.

Original languageEnglish
Article number106966
Number of pages14
JournalAgriculture Ecosystems & Environment
Volume297
Early online date25 Apr 2020
DOIs
Publication statusPublished - 1 Aug 2020

Bibliographical note

Acknowledgements
The authors thank all our colleagues for their help during field survey and laboratory analysis. The authors also thank Prof. Jo Smith and Paul Hallett, School of Biological Sciences, University of Aberdeen for constructive comments and English-language editing which improved the quality of this manuscript. This study was financially supported by the National Natural Science Foundation of China (41571130051, 41977003, 41771251) and the Science and Technology Service Network Initiative of the Chinese Academy of Sciences (No. KFJ-STS-ZDTP-039). Shunhua Yang received the support of China Scholarship Council through UK-China Joint Research and Innovation Partnership Fund PhD Placement Programme (grant No. 201802527019) for a 12-month registered postgraduate study at School of Biological Sciences, University of Aberdeen. During the revising of this manuscript, the world is painfully suffering from the COVID-19. We are grateful to those who are dedicating to fight against the virus. We will overcome it and that success will belong to each of us.

Keywords

  • ACCUMULATION
  • DENITRIFICATION
  • GROUNDWATER
  • LATERAL FLOW
  • NITROGEN-BALANCE
  • NORTH CHINA
  • ORGANIC-CARBON
  • TOPOGRAPHY
  • TRANSPORT
  • Ultisol
  • VADOSE ZONE
  • land-use types
  • nitrate variation
  • regolith
  • slope position

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