4.7 Article

Elemental stoichiometry (C, N, P) of soil in the Yellow River Delta nature reserve: Understanding N and P status of soil in the coastal estuary

Journal

SCIENCE OF THE TOTAL ENVIRONMENT
Volume 751, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.scitotenv.2020.141737

Keywords

Elemental contents; Elemental stoichiometry; Coastal estuary; Yellow River Delta nature reserve

Funding

  1. National Key R&D Program of China [2017YFC0505904]
  2. National Natural Science Foundation of China [41501088, 31870468]

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The study on the Yellow River Delta Nature Reserve revealed high spatial heterogeneity and large variations in soil elemental contents and stoichiometric ratios, with noticeable differences between the old Yellow River Delta and the current Yellow River Delta in terms of nitrogen, phosphorus content, and C:N:P ratios.
The Yellow River Delta Nature Reserve (YNR), which includes two separated regions: part of the old Yellow River Delta (OYD) and part of the current Yellow River Delta (CYD), was established to protect coastal wetlands in the coastal estuary. A total of 120 plots were sampled in the YNR in April 2016, and the spatial patterns of soil C, N and P contents and their stoichiometric ratios (C:N (RCN), C:P (RCP) and N:P (RNP)) were studied and interpolated using the Ordinary Kriging method. Results indicated that the soil elemental contents and stoichiometric ratios showed high spatial heterogeneity and large variations. The mean C:N:P ratio (R-CNP) was similar to 64.7:2.3:1 in OYD, and similar to 64.5:2.0:1 in CYD, respectively, and a well-constrained RCP ratio similar to 65:1 was found in the 0-50 cm soil depth within the YNR. N showed greater variation than C and P. Furthermore, N contents in the 0-5 cm soil layer of OYD were significantly higher than that of CYD (F = 4.79, p = 0.03); RCN in 0-5 cm, 5-10 cm layers of OYD was significantly lower than those in the same layers of CYD (F = 4.75, p = 0.03; F = 5.18, p = 0.02, respectively). RNP in 0-5 cm soil layer of OYD was notably higher than that of CYD (F = 4.88, p = 0.03). These results were due to the combined actions of sedimentation, reclamation and fertilization. Finally, we concluded that a longer reclamation and fertilization history led to decreased RCN in coastal estuary soils, confirmed that the soil of the YNR exhibits N limitation, and suggested that the soil RCN and RNP could be good indicators of the anthropogenic improvement status during soil development in this coastal estuary. (C) 2020 Elsevier B.V. All rights reserved.

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