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Soil Carbon Stock and Soil Characteristics at Tasik Chini Forest Reserve, Pahang, Malaysia

机译:马来西亚彭亨彭亨森林储备土壤碳储量及土壤特性

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This study was carried out to determine soil carbon stock and soil characteristic at Tasik Chini Forest Reserve (TCFR), Pahang. A total of 10 (20 m × 25 m) permanent sampling plot was selected randomly within the area of TCFR. Soil samples were taken from all subplots using dutch auger based on soil depth of 0-20cm, 20-40cm, 40-60cm. Soil parameters determined were size distribution, soil water content, bulk density, organic matter, organic carbon content, pH and electrical conductivity. All parameters were determined following their respective standard methods. Results obtained showed that the soil in TCFR was dominated by clay texture (40%), followed by sandy clay loam (30%), loam (20%). Silty clay, clay loam and sandy loam constitutes about 10% of the soil texture. Range of mean percentage of organic matter and bulk density are from 2.42±0.06% to 11.64±0.39% and 1.01 to 1.04 (gcm~(-3)), respectively. Soil pH are relatively very acidic and mean of electrical conductivity is low. Soil carbon content ranged from 0.83±0.03 to 1.87±0.41%. All soil parameter showed a decreasing trend with depth except electrical conductivity. ANOVA test of mean percentage of organic matter, soil water content, soil pH and electrical conductivity showed a significant difference between plot (p<0.05). However there are no significant difference of mean bulk density between plots (p>0.05). There are no significant difference in mean percentage of soil water content, organic matter and bulk density between three different depth (p>0.05). There were a significant difference on percentage of soil carbon organic between plots and depth. The mean of soil organic carbon stock in soil to a depth of 60 cm calculated was 35.50 t/ha.
机译:本研究进行了达西克森林储备(TCFR),彭港确定土壤碳储量及土壤特性。在TCFR面积内随机选择总共10个(20m×25μm)永久性取样图。根据土壤深度为0-20cm,20-40cm,40-60cm,从所有荷兰螺旋钻取出土壤样品。确定的土壤参数是尺寸分布,土壤含水量,堆积密度,有机物,有机碳含量,pH和导电性。通过各自的标准方法确定所有参数。得到的结果表明,TCFR中的土壤由粘土纹理(40%)主导,其次是砂质粘土壤土(30%),壤土(20%)。粉质粘土,粘土壤土和沙质壤土构成约10%的土壤质地。有机物质的平均百分比范围和堆积密度分别为2.42±0.06%至11.64±0.39%和1.01至1.04(GCM〜(-3))。土壤pH相对非常酸性,电导率的平均值低。土壤碳含量为0.83±0.03至1.87±0.41%。除电导率外,所有土壤参数都表现出降低趋势。 ANOVA测试有机质的平均百分比,土壤含水量,土壤pH和电导率在图之间显示出显着差异(P <0.05)。然而,图之间的平均堆积密度没有显着差异(p> 0.05)。在三种不同深度之间的土壤含水量,有机物和堆积密度的平均百分比没有显着差异(P> 0.05)。地块和深度之间的土壤碳百分比有显着差异。土壤有机碳股在土壤中的平均值为60厘米,计算为35.50吨/小时。

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