. Upslope length improves spatial estimation of soil organic carbon content. Can. J. Soil Sci. 87: 291-300. Quantifying soil organic carbon (SOC) is important to aide in assessing carbon (C) sequestration potential, and as an indicator of soil quality. However, intensive sampling of SOC for quantification can be expensive and time consuming. The objectives of this study were to identify which topographic index correlated best with SOC and determine if incorporating the index improved interpolation of limited SOC data. A transect with 93 sample points spaced 6 m apart was set up, and four topographical indices (curvature, wetness index, upslope length, and elevation) were evaluated for their potential as secondary variables. Three Kriging-based interpolation methods, ordinary kriging, cokriging, and simple kriging with varying local means were compared to determine if incorporating topographical indices improved interpolation of SOC. The upslope length, which takes into consideration the quantity of water that will be redistributed to a point, was found to have the strongest relationship with SOC (R 2 = 0.48, P < 0.01) and was used as a secondary variable for kriging. Thirty points from the SOC data were randomly selected and used in the kriging algorithms to estimate the remaining 63 points. The sum of squared differences (SSD) showed a significant reduction (from 1677 to 1455 for SKlm and from 1677 to 1464 for cokriging) in estimates when upslope length was used as a secondary variable. These results indicate that fewer samples may be taken to estimate SOC accurately and precisely if upslope length is incorporated. On a landscape scale this could facilitate quantification of carbon credits and management decisions in precision farming systems.Key words: Geostatics, kriging, cokriging, organic carbon, landscape processes, wetness index Luca, C., Si, B. C. et Farrell, R. E. 2007. La longueur de la pente ascendante améliore l'estimation spatiale de la concentration du carbone organique du sol. Can. J. Soil Sci. 87: 291-300. Il est important de quantifier la concentration de carbone organique du sol (COS) pour évaluer le potentiel de séquestration du carbone (C) et se faire une idée de la qualité du sol. Le prélèvement d'un grand nombre d'échantillons à cette fin s'avère toutefois aussi onéreux que laborieux. L'étude devait établir quel indice topographique présente la meilleure corrélation avec le COS et si son intégration faciliterait l'interpolation des données sur le COS quand elles sont limitées. Les auteurs ont tracé une ligne de 93 points d'échantillonnage chacun séparés de 6 m et évalué l'utilité de quatre indices topographiques (courbure, indice d'hydratation superficielle, longueur de la pente ascendante et altitude) en tant que variable secondaire. Ils ont ensuite comparé trois méthodes d'interpolation reposant sur le krigeage (krigeage ordinaire, cokrigeage et krigeage simple) avec les moyennes locales pour déterminer si l'intégration des indices topographiques améliore l'interpolation de la concentrati...