Black carbon in urban soils: land use and climate drive variation at the surface

Molly Burke; Erika Marín-Spiotta; Alexandra G Ponette-González

doi:10.1186/s13021-024-00255-3

Black carbon in urban soils: land use and climate drive variation at the surface

Carbon Balance Manag. 2024 Mar 2;19(1):9. doi: 10.1186/s13021-024-00255-3.

Authors

Molly Burke^{1

2}, Erika Marín-Spiotta³, Alexandra G Ponette-González^{4

5

6}

Affiliations

¹ Department of Geography and the Environment, University of North Texas, 1155 Union Circle #305279, Denton, TX, 76203, USA.
² Department of Geography, University of Utah, Salt Lake City, UT, 84112, USA.
³ Department of Geography, University of Wisconsin-Madison, 550 North Park Street, Madison, WI, 53706, USA.
⁴ Department of Geography and the Environment, University of North Texas, 1155 Union Circle #305279, Denton, TX, 76203, USA. alexandra.ponette@utah.edu.
⁵ Department of City and Metropolitan Planning, University of Utah, Salt Lake City, UT, 84112, USA. alexandra.ponette@utah.edu.
⁶ Natural History Museum of Utah, University of Utah, Salt Lake City, UT, 84108, USA. alexandra.ponette@utah.edu.

Abstract

Background: Black carbon (BC) encompasses a range of carbonaceous materials--including soot, char, and charcoal--derived from the incomplete combustion of fossil fuels and biomass. Urban soils can become enriched in BC due to proximity to these combustion sources. We conducted a literature review of BC in urban soils globally and found 26 studies reporting BC and total organic carbon (TOC) content collected to a maximum of 578 cm depth in urban soils across 35 cities and 10 countries. We recorded data on city, climate, and land use/land cover characteristics to examine drivers of BC content and contribution to TOC in soil.

Results: All studies were conducted in the northern hemisphere, with 68% of the data points collected in China and the United States. Surface samples (0-20 cm) accounted for 62% of samples in the dataset. Therefore, we focused our analysis on 0-10 cm and 10-20 cm depths. Urban soil BC content ranged from 0-124 mg/g (median = 3 mg/g) at 0-10 cm and from 0-53 mg/g (median = 2.8 mg/g) at 10-20 cm depth. The median proportional contribution of BC to TOC was 23% and 15% at 0-10 cm and 10-20 cm, respectively. Surface soils sampled in industrial land use and near roads had the highest BC contents and proportions, whereas samples from residential sites had among the lowest. Soil BC content decreased with mean annual soil temperature.

Conclusions: Our review indicates that BC comprises a major fraction (nearly one quarter) of the TOC in urban surface soils, yet sampling bias towards the surface could hide the potential for BC storage at depth. Land use emerged as an importer driver of soil BC contents and proportions, whereas land cover effects remain uncertain. Warmer and wetter soils were found to have lower soil BC than cooler and drier soils, differences that likely reflect soil BC loss mechanisms. Additional research on urban soil BC at depth and from diverse climates is critical to better understand the role of cities in the global carbon cycle.

Keywords: Air pollution; Cities; Land cover; Nature-based solutions; Organic carbon; Pyrogenic carbon; Roads.

Publication types

Review

Grants and funding

1552410/National Science Foundation