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The microstructure of coconut coir dusts for use as alternatives to peat in soilless growing media

机译:椰壳粉尘的微观结构,可替代无土栽培介质中的泥炭

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AbstractnnThe microstructure of the mesocarp pithy tissue and short-length fibres of 2 differently processed coconut coir dusts from Mexico and Sri Lanka was studied using scanning electron microscopy and compared with that of a Sphagnum moss peat. Selected physical properties of these materials were also determined for their use in potting media. The 2 coir dusts did not significantly differ in the microstructural parameters studied, whereas they differed remarkably in their particle size and therefore in their physical properties. Pithy tissue was the major constituent of coir dust. Coarse pithy tissue particles (larger than 1 mm) were highly porous, with an internal porosity of 41.0% by volume. These particles exhibited round-shaped external pores which ranged in diameter from 30 to 80 μm, with an average of 44.3 μm, and which accounted for a relative surface porosity of about 40.9%. By contrast, the cells of Sphagnum peat moss leaves showed oval-shaped pores of 20.1 × 11.5 μm, which accounted for a relative surface porosity of only 12.0%. The internal porosity of peat moss leaves was 51.1% by volume. The retting process (soaking in water) applied to the coconut husks in Sri Lanka partially degraded the pithy tissue and coir fibres. Coir dust from Mexico showed lower water-holding capacity and higher aeration than peat, whereas air–water relationships in coir dust from Sri Lanka were similar to those in peat. Although differences observed in microstructure and porosity characteristics could explain the differential physical properties of the three materials studied, the major reason was the different size distribution of their constituent particles.
机译:摘要使用扫描电子显微镜研究了墨西哥和斯里兰卡的两种不同加工的椰壳粉尘的中果皮微薄组织和短纤维的显微结构,并将其与泥炭藓藓泥炭的显微结构进行了比较。还确定了这些材料在灌封介质中的使用所选择的物理性能。两种椰壳粉尘在所研究的微观结构参数上没有显着差异,但是它们的粒径和因此的物理性质差异显着。麻木组织是椰壳粉尘的主要成分。粗麻布组织颗粒(大于1毫米)是高度多孔的,内部孔隙率为41.0%(体积)。这些颗粒表现出圆形的外部孔,其直径范围为30至80μm,平均为44.3μm,并且占相对表面孔隙率约40.9%。相比之下,泥炭藓苔藓叶子的细胞显示出20.1×11.5μm的椭圆形孔,其相对表面孔隙率仅为12.0%。泥炭藓叶的内部孔隙率为51.1%(体积)。应用于斯里兰卡椰子壳的浸胶过程(浸泡在水中)会部分降解鱼腥组织和椰壳纤维。与泥炭相比,来自墨西哥的椰壳粉尘具有较低的持水能力和较高的通气性,而斯里兰卡的椰壳粉尘中的气水关系与泥炭相似。虽然观察到的微观结构和孔隙率特性的差异可以解释所研究的三种材料的物理性能差异,但主要原因是其组成颗粒的尺寸分布不同。

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