MICROBIAL BIOMASS C AND N, AND MINERALIZABLE-N, IN LITTER AND MINERALSOIL UNDER PINUS-RADIATA ON A COASTAL SAND - INFLUENCE OF STAND AGE AND HARVEST MANAGEMENT
Dj. Ross et al., MICROBIAL BIOMASS C AND N, AND MINERALIZABLE-N, IN LITTER AND MINERALSOIL UNDER PINUS-RADIATA ON A COASTAL SAND - INFLUENCE OF STAND AGE AND HARVEST MANAGEMENT, Plant and soil, 175(2), 1995, pp. 167-177
Microbial biomass C and N, and anaerobically mineralizable-N, were mea
sured in the litter and mineral soil (0-10 cm and 10-20 cm depth) of P
inus radiata plantations in two trials on a nitrogen-deficient coastal
sand. The trials comprised (a) stands of different age (1 to 33 years
), with five of the seven stands studied being second rotation, and (b
) a harvest-management trial, with stands established after different
harvesting treatments of the first-rotation trees and understorey deve
lopment controlled by manual weeding and chemical sprays. The harvest-
management stands were sampled in the fifth year after the second-rota
tion establishment. In the stands of different age, the levels of micr
obial biomass C and N, and also mineralizable-N, in the litter and min
eral soil showed no relationship with tree age and were similar to tho
se in the oldest (33 years) stands of P. radiata. In the harvesting tr
ial, five years after establishment of the second rotation, levels of
microbial N and mineralizable-N in the litter and mineral soil were ge
nerally lowest where whole trees and the original forest floor had bee
n removed; they were higher in associated plots in which the original
forest floor had been removed but fertilizer N was regularly applied.
No marked differences were then found between the other harvest treatm
ents, viz. whole-tree harvest, stem-only harvest with slash remaining
on site, and stem-only harvest plus extra added slash materials. In ea
ch trial, levels of microbial C and N and mineralizable-N were closely
related to total C. and especially total N, in 0-10 cm depth mineral
soil, but not generally in litter. Respiratory measurements strongly s
uggest that the microbial populations in mineral soil had a high metab
olic activity. On an area basis in the harvest-management trial, total
tree N and microbial N in the litter and mineral soil were lowest in
stands where the original forest floor had been removed. In this parti
cular treatment, microbial N in the litter plus mineral soil (0-20 cm
depth) after five years of second-rotation growth comprised 7.3% of th
e total ecosystem N; values in the other treatments ranged between 5.6
and 6.0%. Our results emphasise the importance of slash and litter, a
nd probably volunteer shrubs and herbaceous understorey species, in co
nserving pools of potentially available N during the early stages of t
ree development.