作为西苏门答腊 Pesisir Selatan 地区油棕种植园泥炭地退化生物传感器的漆酶活性研究

Mimien Harianti, Teguh Budi Prasetyo, Lusi Maira, Junaidi Junaidi, H. Herviyanti, Syaiful Anwar, Susilawati Kasim
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引用次数: 0

摘要

这项研究的目的是研究作为油棕种植园泥炭地降解生物传感器的酶活性。研究在西苏门答腊岛的 Pesisir Selatan 进行,研究对象是两块泥炭地,它们的厚度和位置坐标各不相同,即南纬 02o20'07.5",东经 101o00'22",泥炭厚度为 3 米。这两个地点的油棕树龄均为 11 年(种植年份为 2007 年)。采用横断面法对种植园区块的泥炭地进行了观察和取样。横断面垂直于排水渠。泥炭样本在油棕根部(非根层)外采集。观察点距离排水渠边缘分别为 5、15、25、50、75、100、150 米,根系层厚度分别为 0-25 厘米和 25-50 厘米。观察到的泥炭特征包括地下水位、漆酶活性、含水量、pH 值、总铁和铜。一个断面的地下水位在 60-80 厘米之间,仍在可容忍范围内。在 Pesisir Selatan 泥炭地的油棕榈种植园中,作为泥炭降解生物传感器的漆酶活性在 0-25 厘米层中较高,平均小于 0.5 µmol/g。随着离排水渠的距离和泥炭层厚度的增加,含水量的增加降低了漆酶的活性。灰分增加导致铁和铜含量增加,特别是在厚度小于 3 米的泥炭中,可能会抑制漆酶活性。尽管以漆酶活性作为泥炭降解的生物传感器,Pesisir Selatan 油棕种植园的泥炭地在分解过程中仍然相对稳定。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study of Laccase Activity as a Biosensor for Peatland Degradation in Oil Palm Plantations in Pesisir Selatan of West Sumatra
The aim of the research was to study enzyme activity as biosensors for peatland degradation in oil palm plantations. The study was conducted in Pesisir Selatan,West Sumatra, on two peatlands with different thicknesses and location coordinates, namely peat with a thickness of <3 m S: 02o18'45.5", 101o00’37.3” and peat with a thickness >3 m S: 02o20’07.5”, E: 101o00’22”. The oil palm in these two locations is 11 years old (planting year of 2007). Observations and sampling of peatlands were carried out on the plantation blocks using the transect method. The transect was set perpendicular to the drainage canal. Peat samples were collected outside the roots (non-rhizosphere) of oil palm. Observation sites were at a distance of 5, 15, 25, 50, 75, 100, 150 m from the edge of the drainage canal and at the thickness of the root layer of 0-25 and 25-50 cm. Peat characteristics observed were water table level, laccase activity, water content, pH, total Fe, and Cu. The water table level in one transect ranged from 60-80 cm and was still within tolerable limits. The laccase activity as a peat degradation biosensor in oil palm plantations in Pesisir Selatan peatland was higher in the 0-25cm layer with an average of <0.5 µmol/g. The increase in water content decreased the laccase activity along with increasing of the distance from the drainage canal and the thickness of the peat layer. The increase in Fe and Cu resulted from increased levels of ash, particularly in peat with a thickness of <3 m, may suppress laccase activity. Peatland in the oil palm plantation of Pesisir Selatan is still relatively stable despite the decomposition processes characterized by laccase activity as a biosensor for peat degradation.
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