Doi Ryoichi, Ranamukhaarachchi Senaratne Leelananda
Asian Institute of Technology, Klong Luang, Pathumthani 12120, Thailand.
Rev Biol Trop. 2009 Mar-Jun;57(1-2):223-34. doi: 10.15517/rbt.v57i1-2.11317.
Soil dehydrogenase activity is a good indicator of overall microbial activity in soil, and it can serve as a good indicator of soil condition. However, seasonal changes in soil moisture content may have an effect on soil dehydrogenase activity, making an accurate assessment of soil condition difficult. In this study, we attempted to determine the significance of soil dehydrogenase activity for assessing soil condition, and we attempted to find a way to account for the influence of soil moisture content on soil dehydrogenase activity.' Soils were sampled in dry evergreen forest (original vegetation), bare ground (severely degraded) and Acacia plantation plots established on bare ground in 1986 and 1987 in Sakaerat, Thailand. Soil physico-chemical characteristics and dehydrogenase activity in the Acacia plantation soil had few differences from those in the evergreen forest soil. Soil dehydrogenase activity varied significantly between the bare ground and the forests regardless of the season (wet or dry), while the season did not produce a significant variation in soil dehydrogenase activity, as determined by repeated measures analysis of variance (p=0.077). The physico-chemical data provided the first principal component as a good measure of soil fertility. Values of soil dehydrogenase activity significantly correlated to scores of the soil samples of the first principal component (R=0.787, p<0.001). We found that soil dehydrogenase activity is a useful indicator of the extent of soil degradation and the rehabilitative effects of reforestation in this part of Thailand.
土壤脱氢酶活性是土壤中微生物总体活性的良好指标,也可作为土壤状况的良好指标。然而,土壤含水量的季节性变化可能会影响土壤脱氢酶活性,从而难以准确评估土壤状况。在本研究中,我们试图确定土壤脱氢酶活性在评估土壤状况方面的意义,并试图找到一种方法来解释土壤含水量对土壤脱氢酶活性的影响。在泰国呵叻府的萨凯拉特,于1986年和1987年在干燥常绿林(原始植被)、裸地(严重退化)以及在裸地上建立的金合欢人工林地块采集土壤样本。金合欢人工林土壤的理化特性和脱氢酶活性与常绿林土壤的差异不大。无论季节(湿润或干燥)如何,裸地和森林之间的土壤脱氢酶活性差异显著,而重复测量方差分析表明季节对土壤脱氢酶活性没有显著影响(p = 0.077)。理化数据提供了作为土壤肥力良好指标的第一主成分。土壤脱氢酶活性值与第一主成分土壤样本得分显著相关(R = 0.787,p < 0.001)。我们发现土壤脱氢酶活性是泰国这一地区土壤退化程度和重新造林恢复效果的有用指标。