Tree species and diversity effects on soil water seepage in a tropical plantation
Introduction
The area of planted forest increased globally by about 5 million ha per year between 2005 and 2010 and accounts for an estimated 7% (264 million ha) of the total forested area today (FAO, 2010). In Panama, the area of planted forests in 2010 was 79,000 ha, six times larger than in 1990, with an annual growth of 5% over the last 5 years. Today, 44% of the land is still forested and the deforestation rate is low (−0.36% yr−1) (FAO, 2010). It can be expected that with the expanding carbon markets (FAO, 2011) and increasing demands for bioenergy (UN Energy, 2007) the total area of forest plantation will further grow in the near future. Monocultures, for example, of the exotic hardwood tree Tectona grandis L.f. (teak tree) that accounted for 76% of plantations established in Panama between 1992 and 2000, may be very productive, but appear to have drawbacks like promotion of soil erosion and reduction of soil quality (Wishnie et al., 2007). In general, the wide-spread monocultures of exotic species threaten the local biodiversity (Healey and Gara, 2003). Furthermore, it is increasingly reported that plant diversity is crucial for maintaining the function and stability of ecosystems and biogeochemical cycles calling for increased establishment of mixed-species plantations (Loreau et al., 2001).
Global analysis by Jackson et al. (2005) over 504 catchments showed that stream flow decreased dramatically within a few years after setting up plantations, which can impact the water cycle up to 20 years. In the watershed of the Panama Canal, reduction of the water supply due to enhanced evapotranspiration (ET) losses by large scale afforestation might cause limited trafficability of the canal, because the water budget for the canal is tight (Ibanez et al., 2002). However, forests are seen to secure the water supply of the canal by reducing sediment loads and ensuring sufficient dry season flow (Condit et al., 2001, Harmon, 2005).
Because of the growing concern that tree plantations might affect base flow conditions (Malmer et al., 2010, Scott and Prinsloo, 2008), the effect of mixed-species plantations as compared to the traditional monoculture plantations needs to be assessed thoroughly. Surveys over the last decade showed that tree diversity has an impact on ecosystem functioning such as the control of nutrient cycles in a mixed-species tree plantation in Panama (Oelmann et al., 2010, Potvin et al., 2011, Zeugin et al., 2010). From grassland experiments it is further known that plants in mixtures of species are often more productive and have greater water use than in monocultures, which might be related to complementary effects (Caldeira et al., 2001, Verheyen et al., 2008). Recently, Forrester et al. (2010) found higher transpiration rates in mixtures of Eucalyptus globulus Labill. and Acacia mearnsii De Wild, but the mixture also used the water more efficiently. In line with these findings, Kunert et al. (2012) showed for an experimental plantation in Panama that individual tree transpiration is enhanced in mixed-tree stands compared to monocultures, the water use efficiency of five-species mixtures being half that of either monocultures, two- or three-species mixtures. Consequently, mixed-tree stands might increase evaporative water losses following afforestation and thus, pose problems to water supply of the Panama Canal. Because of controversial results on water use of mixed-tree stands, it remains unclear whether tree diversity influences seepage rates during the wet season.
To answer this question, our objectives were to (1) calculate the seepage rates at plots of one, three, and six tree species with two approaches of different complexity and (2), to analyze the effect of the different species and the number of tree species on the seepage rates. Two approaches of water balance assessment were used to test if a simple water balance calculation can predict species specific water fluxes at a tropical plantation for the wet season in 2008 similarly well as a physically based soil water transport model (Hydrus-1D).
Section snippets
Study site
The study site is located in Central Panama (9°19′30″N, 79°38′00″W) roughly 50 km north of Panama City close to the village of Sardinilla. The Smithsonian Tropical Research Institute (STRI) maintains a tree plantation for the “Sardinilla Project”, with the goal to assess the influence of diversity on biogeochemical and water cycles. The site belongs to the Panama Canal catchment and has an altitude of about 70 m above sea level. The climate is semi-humid tropical with a mean annual temperature of
Parameter evaluation
The measured bulk density (BD) of the different plots ranged between 0.79 ± 0.01 and 0.95 ± 0.02 g cm−3, and the mean BD over the entire plantation was 0.84 ± 0.01 g cm−3. In general, the soils of the plots of C. odorata (CO in Fig. 1) stands showed significantly higher BD compared to the other species. BD differed significantly over soil depth with higher values in the subsoil compared to the topsoil (T355 = 2.742, p = 0.006). Exceptions were the two monocultures of L. seemannii (LS in Fig. 1) which do not
Conclusion
The presented study showed that the water balance equation (WBE) was superior to the mechanistic water transport model Hydrus-1D for the available data at the Sardinilla site. While the Hydrus model could not reconcile observations of the soils pressure heads, the WBE approach succeeded in reproducing the relative differences in observed transpiration rates of the tree species and the diversity levels. The seepage below six-species mixtures was lower than under the average monoculture based on
Acknowledgements
We are grateful to José Monteza for maintenance of the experimental plantation and data collection and to Chrystal Healey for installing the piezometers. We thank the Smithsonian Tropical Research Institute, Panama, for its constant support of the Sardinilla Experiment and the processing of research permits. This research was funded by the German Research Foundation (DFG Wi 1601/6-1) which we gratefully acknowledge. Field work of M.S. was funded by the DAAD Promos-Grant. S.W. was funded by the
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