A whole-tree harvest (WTH) was conducted at the Hubbard Brook Experimental Forest, New Hampshire, in 1983-1984 to evaluate changes in the loss and supply of nutrients such as K in response to clear-cutting. The WTH removed 554 mmol m-2 associated with forest biomass. During the first 2 yr following the WTH, there were marked increases in concentrations and fluxes of K in drainage waters (stream efflux 24 mmol m-2 yr-1), coinciding with elevated losses of NO3/-. While these losses decreased within 3 yr, concentrations and fluxes of K remained high in Bs2 horizon soil water and streamwater (10.5 mmol m-2 yr-1) for 10 yr relative to the reference watershed (4.8 mmol m-2 yr-1). Soil exchangeable K pools increased within 3 yr after the WTH. In the high-elevation zone of the watershed, soil pools returned to near-preharvest values after 8 yr. In the remainder of the watershed, exchangeable K pools decreased after 8 yr but remained about 20% above preharvest pools. The increase in exchangeable K in the mineral soil probably contributes to the long-term pattern of elevated K concentrations in streamwater after the WTH. Although stream and WTH removal of K (8.5 mmol m-2 yr-1) was large in comparison to preharvest exchangeable K pools (284 mmol(c) m-2), the increased release of K from mineralization of soil organic matter and weathering resulted in an increase in K on the soil exchange complex (43 mmol m-2 yr-1 in the first 8 yr). The increase in exchangeable K provided an available pool of K for the regrowing vegetation.
|Original language||English (US)|
|Number of pages||11|
|Journal||Soil Science Society of America Journal|
|State||Published - Jan 1 1996|
ASJC Scopus subject areas
- Soil Science