Abstract

Urban soils, like other soils, can be sink or source for atmospheric carbon dioxide, and due to urban expansion, are receiving increasing attention. Studying their highly variable attributes requires high-density sampling, which can hardly be achieved using conventional approaches. The objective of this work was to determine the ability of visible and near infrared reflectance spectroscopy (VNIRS) to quantify soil organic carbon (SOC) concentration (gC kg−1) and stock (gC dm−3, or MgC ha−1 for a given depth layer) in parks and sealed soils of two French cities, Marseille and Nantes, using spectra collected on pit walls or in laboratory conditions (air dried, 2 mm sieved samples).Better VNIRS predictions were achieved using laboratory than in situ spectra (R2 ≈ 0.8–0.9 vs. 0.7–0.8 in validation), and for sample SOC concentration than stock (R2val up to 0.83 in situ and 0.95 in the laboratory vs. 0.78 and 0.89, respectively). Stock was conventionally calculated according to four methods that variably account for coarse particles (>2 mm); and it was better predicted when coarse particles were not taken into account. This was logical using laboratory spectra, collected on 2 mm sieved samples; but concerning in situ spectra, this suggested the operator tended to put the spectrometer beside the coarsest particles during spectrum acquisition. This point is worth considering for urban soils, often rich in coarse particles.Stocks were then aggregated at the profile level: SOC stock prediction was more accurate at profile than sample level when using laboratory spectra (R2val = 0.94 vs. 0.89, respectively), probably due to uncertainty compensation; but this was not the case when using in situ spectra, possibly because samples collected for SOC analysis and corresponding VNIRS scans were not at the exact same location.This work demonstrates VNIRS usefulness for quantifying SOC stock time- and cost-effectively, in urban soils especially.

Highlights

  • Soils represent the largest terrestrial pool of organic carbon and they are in strong interaction with the atmosphere (Jacobson et al, 2000; Scharlemann et al, 2014)

  • Particles > 2 mm represented a noticeable proportion of the studied samples: 232 g kg-1 in average (SD g kg-1); and this proportion tended to be higher in Nantes (284 g kg-1 in average, standard deviation (SD) g kg-1) than in Marseille (148 g kg-1 in average, SD 118 g kg-1), with no clear effect of Quantification of soil organic carbon stock in urban soils using visible and near infrared reflectance spectroscopy (VNIRS) in situ or in laboratory conditions

  • The minimum, maximum, mean and SD of observed sample soil organic carbon (SOC) concentration and stock are presented in Table 2, for Marseille (48 samples including 26 in parks and 22 in fallows) and Nantes (84 samples including 32 in parks, 31 in fallows and 21 in sealed soils), stock being calculated according to Eq

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Summary

Introduction

Soils represent the largest terrestrial pool of organic carbon and they are in strong interaction with the atmosphere (Jacobson et al, 2000; Scharlemann et al, 2014). Quantifying soil attributes in urban areas requires high-density sampling and numerous analyses, which is time consuming and expensive. Most work on SOC quantification by VNIRS has regarded SOC concentration, implying that SOC stock determination would still requires the measurement of soil bulk density. A few pioneering studies have recently demonstrated that VNIRS could be used to quantify SOC stock directly in situ, without having to determine bulk density (Roudier et al, 2015; Cambou et al, 2016). The objective of the present work was to use VNIRS in situ for quantifying SOC concentration and stock for different urban uses (parks, fallows and sealed soils) in two French cities, Marseille and Nantes, which differ in climate, geology and history. Spectra were acquired on air-dried, 2 mm sieved samples to compare predictions made from spectra acquired in situ vs. in laboratory conditions

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