Garcia-Montiel D C, Binkley D
Department of Forest Sciences, Colorado State University, Fort Collins, CO 80523, USA, , , , , , US.
Oecologia. 1998 Feb;113(4):547-556. doi: 10.1007/s004420050408.
This study investigated the differences between two fast-growing tropical tree species on soil N flux and availability. The work was conducted in the island of Hawaii and included three sites located along the Hamakua coast on the northeastern side of the island. Within each site pure stands of Eucalyptus saligna (Sm.)␣and the N2-fixing Albizia falcataria (L.) Fosberg [=Paraserianthes falcataria (L.) Nielsen] were arranged in four randomized complete blocks. For most of the variables considered in this study, the species effects were usually strong and the site effects were significant in some cases. After 13 years, soils under the Albizia stand contained larger pools of total soil C and N, and larger pools of inorganic N. Soil N availability indexed by ion exchange resin bags revealed a strong pattern of species and site effect on N availability; soils under Albizia showed a 2.6-9 fold increase in N availability (P < 0.01). Potential net rates of N transformation (10- and 30-day aerobic incubations) were more than twice as high for soils under the Albizia than under the Eucalytus stands. Nitrogen mineralization during anaerobic incubations were about 10% greater on Albizia soils. Gross microbial mineralization and immobilization were determined by estimating the gross rates of N transformation by the N-isotope pool dilution techniques. Across species and sites, a strong linear positive relationship was obtained for gross immobilization and gross mineralization indicating faster gross immobilization as gross mineralization increases. Soil microbial biomass on Albizia soils contained larger proportion of it as bacterial biomass, while larger proportion of fungi biomass comprised the microbial biomass under Eucalyptus soils. This study clearly showed that the presence of Albizia increased total N pools and N supply to the ecosystem. The overall effect on soil fertility will need to be characterized by the effect of the N-fixer on other nutrients, especially the effect on phosphorus.
本研究调查了两种速生热带树种在土壤氮通量和有效性方面的差异。该研究在夏威夷岛进行,包括位于该岛东北侧哈马库阿海岸沿线的三个地点。在每个地点,将柳桉(Eucalyptus saligna (Sm.))纯林和固氮的南洋楹(Albizia falcataria (L.) Fosberg [=Paraserianthes falcataria (L.) Nielsen])纯林安排在四个随机完全区组中。对于本研究中考虑的大多数变量,物种效应通常很强,地点效应在某些情况下也很显著。13年后,南洋楹林下土壤中总土壤碳和氮的储量更大,无机氮储量也更大。用离子交换树脂袋测定的土壤氮有效性显示,物种和地点对氮有效性有很强的影响模式;南洋楹林下土壤的氮有效性提高了2.6至9倍(P < 0.01)。南洋楹林下土壤的潜在氮转化净速率(10天和30天好氧培养)是桉树林下土壤的两倍多。厌氧培养期间南洋楹土壤中的氮矿化量约高10%。通过氮同位素池稀释技术估算氮转化总速率来测定总微生物矿化和固定作用。在不同物种和地点之间,总固定作用和总矿化作用呈现出很强的线性正相关关系,表明随着总矿化作用的增加,总固定作用加快。南洋楹土壤中的土壤微生物生物量中细菌生物量所占比例更大,而桉树林下土壤中的微生物生物量中真菌生物量所占比例更大。本研究清楚地表明,南洋楹的存在增加了生态系统中的总氮储量和氮供应。固氮树种对其他养分的影响,尤其是对磷的影响,将需要对土壤肥力的总体影响进行表征。