Koga Masaaki, Yoshimura Kazuhisa
Department of Chemistry, Faculty of Sciences, Kyushu University, Fukuoka, Japan 812-8581.
J Environ Monit. 2012 Jul;14(7):1951-8. doi: 10.1039/c2em11003b. Epub 2012 Jun 7.
The phosphate concentration in mountainous stream water can be a measure of the forest condition, because its concentration will be low when the biomass in the forest is increasing and vice versa when the forest is declining. To investigate the seasonal change in the dissolved phosphate concentration of the mountainous stream water of the Yamakami River, Kitakyushu, from June 2009 to August 2010, and the regulation mechanism of the phosphate concentration, solid-phase spectrophotometry, which can be applicable to natural water without any pretreatment procedures, was employed for the determination of phosphate at μg P L(-1) levels in natural water. The phosphate concentrations in the mountainous stream waters at 6 sites ranged from 2.2 to 13 μg P L(-1), and those from the catchment area of the steady state forest were 5.3 ± 1.6 (±1 SD) μg P L(-1). Changes in the concentration were fairly small even during a storm runoff. The average phosphate concentration of rain was 2.8 ± 0.7 μg P L(-1), about half of the concentration in the stream water. The rate of runoff in forest areas is generally considered to be about 50% of the total precipitation. For a forest under a climax condition, the phosphate concentration is estimated to be regulated by the fallout and evapotranspiration (α = 0.05). At one of the sites, an upstream tributary, where a fairly big landslide occurred before July in 2009, the phosphate concentration was the highest, suggesting that the biomass may still be decreasing. For all of the six sites examined, a characteristic seasonal change in phosphate concentration was observed, reflecting the local budget between the biological decomposition of plant matter and the consumption by the biomass. The increase in the phosphate concentration during late spring and early summer may result from the extensive decomposition of plant litter mainly supplied in autumn and of plant matter relating to spring blooming such as fallen flowers, pollen and immature fruits. The proposed method using the phosphate concentration in surface stream waters without the period of the seasonal change mentioned above is expected to be very helpful in diagnosing the condition of forests.
山区溪水中的磷酸盐浓度可作为森林状况的一种衡量指标,因为当森林生物量增加时其浓度会降低,反之,当森林衰退时其浓度会升高。为了研究2009年6月至2010年8月期间北九州市山间河流矢上川溪水中溶解磷酸盐浓度的季节变化以及磷酸盐浓度的调节机制,采用了无需任何预处理程序即可应用于天然水的固相分光光度法,用于测定天然水中微克磷每升水平的磷酸盐。6个采样点的山区溪水中磷酸盐浓度范围为2.2至13微克磷每升,来自稳定状态森林集水区的浓度为5.3±1.6(±1标准差)微克磷每升。即使在暴雨径流期间,浓度变化也相当小。雨水的平均磷酸盐浓度为2.8±0.7微克磷每升,约为溪水中浓度的一半。一般认为森林地区的径流率约为总降水量的50%。对于处于顶级群落状态的森林,估计磷酸盐浓度受沉降和蒸散作用调节(α=0.05)。在其中一个采样点,即2009年7月前发生较大山体滑坡的上游支流处,磷酸盐浓度最高,这表明生物量可能仍在减少。在所考察的所有6个采样点,均观察到磷酸盐浓度具有特征性的季节变化,反映了植物物质生物分解与生物量消耗之间的局部平衡。晚春和初夏期间磷酸盐浓度的升高可能是由于主要在秋季供应的植物凋落物以及与春季开花相关的植物物质(如落花、花粉和未成熟果实)的大量分解所致。利用上述无季节性变化时期的地表溪水中磷酸盐浓度的方法有望对森林状况诊断非常有帮助。