Changes in biogeochemical cycling following forest defoliation by pine wilt disease in Kiryu experimental catchment in Japan

Abstract

AbstractChanges in nutrient budgets and hydrological processes due to the natural disturbance of pine wilt disease (PWD) were monitored in a small, forested watershed in Japan. The disturbance caused changes in soil nitrogen transformations. Pre‐disturbance, mineralized nitrogen remained in the form of NH4+, whereas in disturbed areas most mineralized nitrogen was nitrified. Stream NO3− concentrations increased following PWD. There was a delay between time of disturbance and the increase of NO3− in ground and stream waters. Stream concentrations of NO3− and cations (Ca2+ + Mg2+) were significantly correlated from 1994 to 1996, whereas the correlation among NO3−, H+, and SO42− was significant only in 1995. Although both cation exchange and SO42− adsorption buffered protons, cation exchange was the dominant and continuous mechanism for acid buffering. SO42− adsorption was variable and highly pH dependent. The disturbance also resulted in slight delayed changes of input–output nutrient balances. The nitrogen contribution to PWD litter inputs was 7·39 kmol ha−1, and nitrogen loss from streamwater was less than 0·5 kmol ha−1 year−1 throughout the observation period. This large discrepancy suggested substantial nitrogen immobilization. Copyright © 2004 John Wiley & Sons, Ltd.