Premium
Nutrient Accumulation and Cycling in Loblolly Pine (Pinus taeda L.) Plantation Ecosystems: The First Twenty Years
Author(s) -
Switzer G. L.,
Nelson L. E.
Publication year - 1972
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj1972.03615995003600010033x
Subject(s) - nutrient , nutrient cycle , biogeochemical cycle , loblolly pine , cycling , pinus <genus> , environmental science , perennial plant , ecosystem , agronomy , ecology , chemistry , botany , biology , forestry , geography
The mass of the system increased by 10‐fold during this period; and in terms of the system's initial nutrient fund, the quantities of N, P, K, Ca, Mg, and S increased approximately 4, 4, 11, 7, 5, and 3 times, respectively. The quantity of nutrients present in the above ground portion of the system at 20 years ranges from 298 for N to 24 kg/ha for S, about a 12‐fold difference. The portion of the system's total nutrient fund that is cycling to meet the annual requirement during the 20th year is small, ranging from a minimum of 7% for Ca to a maximum of 28% for K. This range is principally a reflection of the disposition and mobility of the nutrients. A technique of accounting for the system's nutrient budget is developed and an example presented. This technique indicates that, with some nutrients in these perennial systems, a sizable portion of the annual requirements is met by transfer within the living fraction of the system. Thus, in addition to the geochemical and biogeochemical cycles, a biochemical cycle is proposed which encompasses the internal transfer relationships or translocations of nutrients within the trees. Consideration of this phenomena leads to a more realistic concept of nutrient cycling within these and similar systems.