14 research outputs found

    Soil Organic Carbon depth profiles in relation to topographic parameters

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    We have to understand the spatial dynamics (horizontally and vertically) of the store of the Soil Organic Carbon (SOC) to manage soil resource. At large scale, a broad range of parameters is typically required. But regarding a smaller scale the bedrock and soils types are more homogenous. This study aims to characterize the relation of the vertical distribution of SOC content and the topography at the farm scale. For that, we sampled 19 cores up to 1m depth in different topographical contexts. We measured by spectroscopy the SOC content each 3cm along the core to establish a high resolution vertical distribution which we summa-rized by fitting of a cubic function. We show that these parameters are well explained by the slope and curva-ture (mean R² c. 0.5 for all parameters). These correlations were used to map the SOC content at GlobalSoil-Map depth layers

    Broad-scale soil monitoring schemes

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    Soil resources provide many important ecosystem goods and services. However, they are at risk from a variety of threats operating over a broad range of scales. Political awareness that soil is threatened by increasing pressures has been rising for several years (European Commission 2006). Indeed, the demand for soil information is increasing continuously (Richer de Forges and Arrouays 2010). Although rates of soil degradation are often slow and only detectable over long timescales, they are often irreversible. Therefore, monitoring soil quality and condition is essential in order to detect adverse changes in their status at an early stage

    Farm-Scale Soil Carbon Auditing

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    The soil system is recognized as a significant terrestrial sink of carbon. Estimates for the top meter of soil in the world range between 1,200 and 2,500 petagrams for organic C (Batjes 1996; Lal 2004). The reliable assessment and monitoring of soil carbon stocks is of key importance for soil conservation and in mitigation strategies for increased atmospheric carbon (Stockmann et al. 2013). Carbon credits are the heart of a cap-and-trade scheme, by offering a way to quantify carbon sequestered from the atmosphere; carbon credits gain a monetary value to offset a given amount of carbon dioxide releases (Paustian et al. 2009). The agricultural industry worldwide has the capacity to capture and store carbon emissions in soil (Paustian et al. 2000). However, there is still a debate on how soil can benefit for the offsets in the carbon economy because there is no good and efficient way of measuring soil carbon storage with appropriate statistical confidence (Post et al. 2001; Smith 2004b). A scheme that can measure and monitor soil carbon storage on a farm, which is crucial to the participation of the agricultural sector in the carbon economy, is essential
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