Estimation of soil erosion rates in dehesas using the inflection point of holm oaks

• Published in: Catena (Giessen) 2018-07, Vol.166, p.56-67
• Main Authors: Rubio-Delgado, Judit, Schnabel, Susanne, Gómez-Gutiérrez, Álvaro, Sánchez-Fernández, Manuel
• Format: Article
• Language: English
• Subjects: Basal growth; Partially exposed roots; Rangelands; Soil erosion; Southwest Spain; Terrestrial laser scanning
• ISSN: 0341-8162; 1872-6887
• DOI: 10.1016/j.catena.2018.03.017

The exposure of tree or shrub roots represents a clear indicator of soil loss in the surrounding area. Previous studies have used this type of botanical evidence to estimate soil erosion rates, preferring roots at some distance from the tree stem because the inflection point (or root collar) undergoes a vertical displacement caused by basal growth. The aim of this paper is to develop a method that combines the inflection point of holm oaks and high-resolution digital images obtained by means of a terrestrial laser scanner to estimate soil erosion rates in Mediterranean dehesas. To correct for vertical displacement, the basal growth of each tree was determined in the field, differentiating the part of the roots that had been exposed by erosion from that generated by wood growth. Two datasets obtained through different approaches were used for validating the basal growth measured in the field survey: (i) a growth study analysing stems and cores of holm oaks and (ii) field measurements of basal growth of holm oaks located in an area without soil erosion. The results obtained by each method offered similar mean values (12.7 and 8.4 cm, respectively) as compared to the values estimated in the field survey (10.2 cm). Afterwards, soil erosion rates were corrected, reducing the values on average by 40%, with a mean loss of 26.7 t ha‐1 y−1. No relationship was found between tree age and basal growth. On the other hand, soil erosion rates showed a slightly negative trend with relation to tree age, indicating an upward tendency of soil losses from the year 1640 to 2014. Finally, it was possible to define three periods with varying erosion rates: 10.4 t ha−1 y−1 (1640–1830), 19.2 t ha−1 y−1 (1831–1888) and 27.2 t ha−1 y−1 (1889–2014). •Soil erosion rates can be estimated combining the inflection point method and laser scanner images.•The correction of the basal growth reduces the rates by approximately 40%, avoiding overestimation.•The inflection point method is a non-invasive technique to estimate soil erosion rates.•Soil erosion rates showed a continuous increase since the second half of the 17th century.•Soil erosion rates are highly variable in space.