The distribution of solute processes on an acid hillslope and the delivery of solutes to a stream: I. Exchangeable bases

✍ Scribed by Burt, T. P.; Park, S. J.

• Publisher: John Wiley and Sons
• Year: 1999
• Tongue: English
• Weight: 827 KB
• Volume: 24
• Category: Article
• ISSN: 0360-1269
• DOI: 10.1002/(sici)1096-9837(199908)24:9<781::aid-esp10>3.0.co;2-l

✦ Synopsis

This paper aims to identify the spatial distribution of exchangeable base cations in soils on an acid hillslope and to investigate possible cation release processes from slope soils to the stream. The basic assumption underlying this research is that the amount of exchangeable cations in soils reflects the nutrient stores and cation leaching processes across the slope where vegetation and parent materials are similar. The distribution of exchangeable Ca 2 , Mg 2 , K and Na has been investigated on a three-dimensional hillslope on the Quantock Hills, Somerset, UK. A two-way ANOVA shows that soil depth is predominant in explaining the total variance of exchangeable bases, despite the steep slope gradient and clear podzolic catena development. Major nutrient base cations, such as Ca 2 , Mg 2 and K , display homogeneous topsoil storage right across the slope. This spatial pattern may indicate that the spatial distribution of major nutrient cations is tightly controlled by the soil±vegetation system in nutrient-poor heathland environments. Na is an exception to this vegetationcontrolled spatial distribution, because of its small involvement in the soil±vegetation and soil exchangeable systems. In subsurface soils, cations liberated from the soil±vegetation system are subject to redistribution over the slope according to the hydrological flowpaths operating on the slope, with some eventually released into the stream. The saturated wedge developed at the base of the slope plays a key role in the storage and release processes of base cations from slope soils to the stream. Ca 2 , Mg 2 and Na carried by throughflow are stored in the saturated wedge and gradually released into the stream at times of high flow. K , however, shows an apparently different spatial behaviour, being deficient in the saturated wedge.