The effects of phytophagous insects on water and soil nutrient concentrations and fluxes through forest stands of the Level II monitoring network in the UK

• Published in: The Science of the total environment 2010-12, Vol.409 (1), p.169-181
• Main Authors: Pitman, R.M., Vanguelova, E.I., Benham, S.E.
• Format: Article
• Language: English
• Subjects: Animal and plant ecology; Animal, plant and microbial ecology; Animals; Aphididae; Biological and medical sciences; Cinara pilicornis; Elatobium abietinum; Environmental Monitoring; Fluxes; Forest monitoring; Forestry; Forests; Fresh Water - chemistry; Fundamental and applied biological sciences. Psychology; General forest ecology; Generalities. Production, biomass. Quality of wood and forest products. General forest ecology; Insecta - metabolism; Insecta - physiology; Insects; K flux; Microorganisms; Monitoring; Nitrogen - analysis; Nitrogen - metabolism; Nitrogen Cycle; Nutrients; Oak; Operophtera brumata; Sitka spruce; Soil (material); Soil - chemistry; Soil Pollutants - analysis; Soil Pollutants - metabolism; Soil type; Soil water NO 3–N; Spruce aphid; Stands; Supports; Synecology; Terrestrial ecosystems; Throughfall DOC flux; Tortrix viridana; Total N flux; Trees - chemistry; Trees - metabolism; United Kingdom; Water quality; Winter moth
• ISSN: 0048-9697; 1879-1026
• DOI: 10.1016/j.scitotenv.2010.09.029

The effects of insect defoliators on throughfall and soil nutrient fluxes were studied in coniferous and deciduous stands at five UK intensive monitoring plots (1998 to 2008). Links were found between the dissolved organic carbon (DOC), nitrogen (N) and potassium (K) fluxes through the forest system to biological activity within the canopy. Underlying soil type determined the leaching or accumulation of these elements. Under oak, monitored at two sites, frass from caterpillars of Tortrix viridana and Operophtera brumata added direct deposition of ~ 16 kg ha −1extra N during defoliation. Peaks of nitrate (NO 3–N) flux between 5 and 9 kg ha −1 (×5 usual winter values) were recorded in consecutive years in shallow soil waters. Synchronous rises in deep soil NO 3–N fluxes at the Grizedale sandy site indicate downward flushing, not seen at the clay site. Under three Sitka spruce stands, generation of honeydew (DOC) was attributed to two aphid species ( Elatobium abietinum and Cinara pilicornis) with distinctive feeding strategies. Throughfall DOC showed mean annual fluxes (6 seasons) ~ 45–60 kg ha −1 compared with rainfall values of 14–22 kg ha −1. Increases of total N in throughfall and NO 3–N fluxes in shallow soil solution were detected — soil water fluxes reached 8 kg ha −1 in Llyn Brianne, ~ 25 kg ha −1 in Tummel, and ~ 40 kg NO 3–N ha −1 in Coalburn. At Tummel, on sandy soil, NO 3–N leaching showed increased concentration at depth, attributed to microbiological activity within the soil. By contrast, at Coalburn and Llyn Brianne, sites on peaty gleys, soil water NO 3–N was retained mostly within the humus layer. Soil type is thus key to predicting N movement and retention patterns. These long term analyses show important direct and indirect effects of phytophagous insects in forest ecosystems, on above and below ground processes affecting tree growth, soil condition, vegetation and water quality.