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Spatial distribution of sediments and transfer properties in soils in a stormwater infiltration basin 总被引：3，自引：2，他引：1
Patrice Cannavo Laure Vidal-Beaudet Béatrice Béchet Laurent Lassabatère Sylvain Charpentier 《Journal of Soils and Sediments》2010,10(8):1499-1509
Purpose
The aim of our study was to characterise the heterogeneity of sediment distribution in a stormwater retention/infiltration basin (Pont de Cheviré, Nantes, France) and to determine the impact of this distribution on water transfer properties in the soil. 相似文献2.
Cambou Aurélie Saby Nicolas P.A. Hunault Gilles Nold François Cannavo Patrice Schwartz Christophe Vidal-Beaudet Laure 《Journal of Soils and Sediments》2021,21(2):1038-1052
Journal of Soils and Sediments - Assessments of urban soil organic carbon stock (SOCS) are scant because citywide data are scarce. Moreover, we do not know which factors mostly explain SOCS spatial... 相似文献
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Bouzouidja Ryad Béchet Béatrice Hanzlikova Jitka Sněhota Michal Le Guern Cécile Capiaux Hervé Jean-Soro Liliane Claverie Rémy Joimel Sophie Schwartz Christophe Guénon René Szkordilisz Flora Körmöndi Barnabas Musy Marjorie Cannavo Patrice Lebeau Thierry 《Journal of Soils and Sediments》2021,21(5):1909-1927
Journal of Soils and Sediments - In urban areas, soil functions are deeply impacted by all human activities, e.g., water infiltration, carbon storage, and chemical substances degradation potential.... 相似文献
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Kristell Hergoualc'h Jean-Michel Harmand Patrice Cannavo Ute Skiba Robert Oliver Catherine Hnault 《Soil biology & biochemistry》2009,41(11):2343-2355
Soil moisture and gaseous N-flux (N2O, N2) dynamics in Costa Rican coffee plantations were successively simulated using a mechanistic model (PASTIS) and two process-based models (NGAS and NOE). Two fertilized (250 kg N ha−1 y−1) coffee plantations were considered, namely a monoculture and a system shaded by the N2 fixing legume species Inga densiflora. In situ N2O fluxes were previously measured in these plantations. NGAS and NOE used specific microbial activities for the soils. To parameterize NGAS, we estimated N mineralization via in situ incubations and the contribution of heterotrophic soil respiration to total soil respiration. Potential denitrification rates and the proportion of denitrified N emitted as N2O were measured in the laboratory to define the values of NOE parameters, as well as nitrification rates and related N2O production rates for parameterizing both models. Soil moisture and both NGAS and NOE N2O fluxes were best modelled on an hourly time step. Soil moisture dynamics were satisfactorily simulated by PASTIS. Simulated N2O fluxes by both NGAS and NOE (3.2 and 2.1 kg N ha−1 y−1 for NGAS; 7.1 and 3.7 kg N ha−1 y−1 for NOE, for the monoculture and shaded plantations respectively) were within a factor of about 2 of the observed annual fluxes (4.3 and 5.8 kg N ha−1 y−1, for the monoculture and shaded plantations respectively). Statistical indicators of association and coincidence between simulated and measured values were satisfactory for both models. Nevertheless, the two models differed greatly in describing the nitrification and denitrification processes. Some of the algorithms in the model NGAS were apparently not applicable to these tropical acidic Andosols. Therefore, more detailed information about microbial processes in different agroecosystems would be needed, notably if process-oriented models were to be used for testing strategies for mitigating N2O emissions. 相似文献
5.
Deniz Yilmaz Patrice Cannavo Geoffroy Séré Laure Vidal-Beaudet Michel Legret Olivier Damas Pierre-Emmanuel Peyneau 《Journal of Soils and Sediments》2018,18(2):442-455
Purpose
The densification and expansion of urban areas will increase the streams of waste materials such as bricks, concrete and street sweeping waste. In parallel, green areas offer the potential to overcome many challenges that face growing/expanding cities but require the use of large amounts of natural resources such as natural topsoil and aggregates. In this work, various waste materials mixed with organic debris are tested for greening applications in urban environments as an alternative to the consumption of natural resources.Materials and methods
Five combinations of artefacts were studied either as “growing material” (i.e. dedicated to plant growth) or “structural material” (as support for traffic). These constructed Technosols were studied in situ in lysimeters under two sets of contrasting climatic conditions at two sites in France (Angers, oceanic climate, and Homécourt semi-continental climate). They were planted with trees (Acer platanoides) and with ryegrass (Lolium perenne L.).Results and discussion
Compared to natural soils, the constructed Technosols exhibited high porosities and highly saturated hydraulic conductivities (up to 0.76 m3 m?3, and to 34.74 cm h?1, respectively). The physical properties–i.e. macroporosity and microporosity–of these artificial soils revealed high water supply for plants, with available soil water ranging from 0.5 to 2.9 mm cm?1. Tree and ryegrass roots were able to grow in the entire soil volume available in the lysimeters. Organic matter nature and soil pH conditions appeared to be the main drivers of plant development.Conclusions
Constructed Technosols are suitable for vegetation growth and constitute a valuable alternative to the consumption of natural arable earth for urban greening applications, e.g. gardens, parks, and tree lines. Furthermore, they can provide high levels of relevant ecosystem functions in cities such as water retention and infiltration, plant settlement, carbon sequestration and even biodiversity habitats.6.
Fourvel Gaëtan Jules Vidal-Beaudet Laure Le Bocq Agathe Thery François Brochier Violaine Cannavo Patrice 《Journal of Soils and Sediments》2019,19(8):3178-3192
Purpose
Fine sediment accumulates upstream of hydroelectric dams. To ensure that dams can operate properly, part of the sediment has to be dredged and land managed. In parallel, using topsoil from agricultural parcels for urban greening or land restoration is currently controversial because arable surface areas are decreasing. An alternative idea for protecting these natural resources consists in reusing fine dredged sediment to construct multifunctional soils. This agronomic use is only possible if sediment can provide acceptable physical and chemical properties for plant growth.
Materials and methodsFour dredged sediments with contrasted initial agronomic properties and one control soil were mixed or not with green waste compost (40% v/v) and used to construct triplicate 30-cm depth soils in lysimetric containers (1.11?×?0.71 m). The 30 constructed soils were exposed to the in situ conditions and sown with ryegrass (Lolium perenne). The evolution of soil chemical and physical properties and plant development were studied every 6 months for 18 months.
Results and discussionAbove- and below-ground biomass production of the constructed soils contrasted according to the sediment properties and to compost addition. A statistical approach identified eight soil parameters linked to biomass production. Among these parameters, soil structure, quantified from aggregate stability, played a fundamental role. A focus on physical properties confirmed that some sediments were only partially adapted to ryegrass support. Compost addition improved sediment physical properties over time, but caused temporary N deficiency during the first months after installation which limited shoot biomass production. Exogenous plant species developed on the constructed Technosols, especially on the soils where the lack of structure and N deficiency had the strongest effect.
ConclusionsAll sediments were suitable for plant growth over the 18 months of the study. A few soil properties emerged as markers of the fertility of sediment-made Technosols. Among them, the soil structure was one of the most determining parameters. It can be assessed by measuring aggregate stability, macroporosity, the crustability index, and bulk density, while available nutrients (N, P, K) and pH seem sufficient to assess chemical fertility. The balance between the properties of the sediment-made Technosols and the needs of the plants seems to be an essential lever for the establishment of functional soil-plant systems for urban greening or for ecological restoration.
相似文献7.
In situ and laboratory measurements of aerobic respiratory and denitrifying activities were studied in the vadose zone (almost 2.5 m thick) of a fluvic hypercalcaric cambisol characterized by transitory anaerobic conditions. A field experiment was conducted in a bare soil, over a 7-month period starting just after maize harvest and incorporation of maize crop residues. Weather variables (air and soil temperature, rainfall), soil water content, soil solutes (NO3− and dissolved organic carbon) and soil gases (CO2 and N2O), were recorded throughout the experiment. Four soil layers were defined. Bacterial counts were performed in each layer using the most probable number (MPN) method. Aerobic respiratory and denitrifying activities were estimated from laboratory measurements. In situ microbial activity, as revealed by CO2 and N2O measurements in the soil atmosphere, was strongly influenced by weather. Laboratory measurements showed that potential aerobic respiratory activity (ARA) occurred throughout the soil profile, whereas semi-potential denitrifying activities SPDA (i.e. measured under organic-C limiting condition) occurred mainly in the top 30 cm soil layer. In the soil profile, the CO2 concentration gradient was stronger than the N2O concentration gradient. Seasonal variations in microbial activities increased with depth, whereas DOC concentrations, and variations in those concentrations, decreased with depth, suggesting that DOC quality investigations are necessary in the deep vadose zone to understand microbial activities seasonal variations. Laboratory measurements of potential activities agreed well with in situ microbial activity in natural environmental conditions. NO3− was a stronger limiting factor for SPDA than was denitrifier density in the soil profile. 相似文献
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Sustainability of urban soils lies in their ability to facilitate water and air permeabilities. Exogenous organic matter has been shown to have a positive impact on these properties. Under urban conditions, a large one‐time input of an organic amendment was made to the reconstituted soil. Two organic materials, green‐waste compost (gw) or cocompost from sewage sludge and wood chips (sw), were mixed with sandy loam soil (40% v/v) and placed in 600‐L containers. Containers received a 29‐cm thick layer of sandy loam soil–organic matter mix over a 28‐cm thick layer without organic amendment. Volumetric water content, dry bulk density, hydraulic conductivity at saturation and water retention were measured over 5 yrs in the soils and values for the mixes and a control compared. After this time, dry bulk density was greater (1.54 g/cm3) in control than in gw or sw soils (1.31 and 1.11 g/cm3, respectively), whereas hydraulic conductivity at saturation was smaller (4 × 10?7 m/s) than in gw (3.4 × 10?6) or sw (3.7 × 10?6 m/s). HYDRUS 1D water balance model indicated that below 27 cm depth in the control after 5 yrs, there was a high degree of anoxia, lasting >200 days per year, compared with <40 days in gw and sw. Amplification of the risk of anoxia below 27 cm depth after 10 yrs was 323, 151 and 100 days in the control, gw and sw, respectively. Organic matter amendment could support sustainable urban soils for ten years after soil reconstitution. 相似文献
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Anaïs Coulon Amelène El-Mufleh Patrice Cannavo Laure Vidal-Beaudet Béatrice Béchet Sylvain Charpentier 《Journal of Soils and Sediments》2013,13(3):508-518
Purpose
In stormwater infiltration basins, sediments accumulate at the soil surface and cause a gradual filling up of soil pores. These sediments are composed of a mixture of natural and anthropogenic (as oil products) organic matters (OMs). The degradation kinetics of these sediment OMs and their biological stability has been neglected. This study aimed to characterize sediments OMs to assess their evolution and their capacity to degrade.Materials and methods
To characterize OMs from the sediment layer, we measured at several places in the infiltration basin, total OM and carbon (C) contents, C distribution and biochemical fractions of the OM in the different size fractions, the sediment’s C mineralization potential, soil microbial biomass, and organic pollutants (polycyclic aromatic hydrocarbons (PAHs)) in the sediment layer.Results and discussion
OM contents were high and varied from 66 to 193 g?kg?1 from the inlet to the outlet of basin. Depending on rainfall intensity and volume, organic particles were deposited at varying distances in the basin by decantation; this was confirmed by analysis of sediment C distribution in the different size fractions. Despite high amounts of OM, organic C had a low biodegradability. Mineralization potentials were low compared to natural soil (i.e., from 0.3 to 1.1 g CO2–C kg?1 total organic carbon). Biochemical fractionation of the organic fractions indicated that they were mainly composed of a soluble fraction, which contributed to reducing OM biodegradability. The activity of the sediment microbial biomass was low. PAH contents seemed to be partly responsible for the high biostability of OMs.Conclusions
There was limited capacity for biodegradation of sediment OMs probably due to inhibitory effects of soluble PAHs and consequently low microbial activity. 相似文献
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