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作 者:石风善[1]
机构地区:[1]黑龙江省农业科学院合江农业科学研究所,黑龙江佳木斯154007
出 处:《草原与草坪》2004年第2期31-33,共3页Grassland and Turf
摘 要:对不同建植年限的多年生草坪土壤进行了物理性状的研究,结果表明,降雨时多年生草坪土壤的水分主要容纳在0~10cm层土壤中;多年生草坪土壤0~10cm层的孔隙度明显大于10~30cm层土壤,并且随着草坪建植时间的增加,0~10cm层的土壤孔隙度有逐渐下降的趋势;多年生草坪0~10cm层的土壤硬度比10~30cm层的大;建植多年生草坪时土壤应采用壤土为宜。The soil physical properties of perennial turf at different age were studied and the results showed that the soil water was mainly held in 0~10 cm horizon when rainfall; the porosity of 0~10 cm horizon was greater than 0~30 cm.At the same time, the soil porosity of 0~10 cm decreased gradually along with the age of turf.The soil hardness of 0~10 cm horizon was greater than 10~30 cm. The loam soil was the best for turf establishment.
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