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February 2, 2026Soil Systems2 citationsOpen Access

The Variation and Driving Factors of Soil Organic Carbon Stocks and Soil CO2 Emissions in Urban Infrastructure: Case of a University Campus

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VVViacheslav VasenevRVR. van VelthuijsenMHMarcel R. Hoosbeek

Key Points

  • The aim is to explore the variation of soil organic carbon stocks and carbon dioxide emissions in urban green infrastructures on a university campus.
  • Conducted random stratified topsoil sampling across the campus area (n = 90)
  • Analyzed SOC profile distribution and fractionation in key sites (n = 8)
  • Measured soil CO2 emissions, temperature, and moisture
  • SOC contents ranged from 1.1 to 5.5% across sampling sites
  • SOC stocks under trees and shrubs were 10–15% higher than under lawns and herbs
  • High CO2 emissions observed under lawns correlated with labile SOC fraction
  • Strong relationship (R2 = 0.71–0.88) between soil temperature and CO2 emissions in lawns
  • Identified hotspots of rapid carbon turnover in recent and intermediate lawns

Abstract

The development of urban green infrastructures (UGI) is considered among the main nature-based solutions for climate mitigation in cities; however, the role of soils in the carbon (C) balance of UGI ecosystems remains largely overlooked. Urban green spaces are typically dominated by constructed Technosols, created by adding organic materials on top of former natural or agricultural subsoils. The combined effects of land-use history and current UGI management result in a high spatial variation of soil organic carbon (SOC) stocks and soil CO2 emissions. Our study aimed to explore this variation for the case of Wageningen University campus. Developed on a former agricultural land, the campus area includes green spaces dominated by trees, shrubs, lawns, and herbs, with well-documented management practices for each vegetation type. Across the campus area (~32 ha), a random stratified topsoil sampling (n = 90) was conducted to map the spatial variation of topsoil (0–10 cm) SOC stocks. At the key sites (n = 8), representing different vegetation types and time of development (old, intermediate, and recent), SOC profile distribution was analyzed including SOC fractionation in surface and subsequent horizons, as well as the dynamics in soil CO2 emissions, temperature, and moisture. Topsoil SOC contents on campus ranged from 1.1 to 5.5% (95% confidence interval). On average, SOC stocks under trees and shrubs were 10–15% higher than those under lawns and herbs. The highest CO2 emissions were observed from soil under lawns and coincided with a high proportion of labile SOC fraction. Temporal dynamics in soil CO2 emissions were mainly driven by soil temperature, with the strongest relation (R2 = 0.71–0.88) observed for lawns. Extrapolating this relationship to the calendar year and across the campus area using high-resolution remote sensing data on surface temperatures resulted in a map of the CO2 emissions/SOC stocks ratio, used as a spatial proxy for C turnover. Areas dominated by recent and intermediate lawns emerged as hotspots of rapid C turnover, highlighting important differences in the role of various UGI types in the C balance of urban green spaces.

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Cite This Study

Vasenev et al. (2026) studied this question.

synapsesocial.com/papers/6980fcb6c1c9540dea80e8f1https://doi.org/10.3390/soilsystems10020024
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