THE BIOGEOCHEMICAL EFFECTS OF THE HEMLOCK WOOLLY ADELGID ON SOIL WATER CHEMISTRY
Ecological effects of hemlock mortality have been investigated, but soil chemistry and soil water chemistry have not been studied in New York. The goal of this study is to investigate the biogeochemical effects of HWA on soil water chemistry using samples from two locations in New York (MK in Blenheim; RVR in Davenport). Three sampling sites were established at MK, a HWA infected site (HWA), a HWA uninfected site (NHWA), and a HWA infected and treated with insecticides site (HWAT). Surface water samples were collected at RVR. Field parameters such as pH, electrical conductivity (EC), dissolved oxygen, temperature, and turbidity were measured on site. Samples were collected every week through the summers of 2014 and 2015. In the lab, cation and anion composition of the water samples were determined using spectroscopy and chromatography techniques.
Chloride, sulfate and bicarbonate are the major anions, and calcium, magnesium and sodium are the major cations in both the surface and soil waters at all sites. None of the water samples have detectable phosphate, while nitrate ranges between 0.180 and 2.61 mg/L at MK and non-detectable at RVR. Potassium concentrations are below detection limit for most samples. pH values are close to neutral in all samples, while the EC values are higher in soil water samples than in the surface water samples. Soil water samples have about ten times more bicarbonate than the surface samples. This collected baseline data provides information to determine any biogeochemical changes which may result from infection of HWA.