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›› 2007, Vol. 43 ›› Issue (zk): 43-47.

• 论文及研究报告 • 上一篇    下一篇

北京西山油松栓皮栎混交林的土壤水分特征

聂立水1 李吉跃2 戴伟1   

  1. 1.北京林业大学水土保持学院,北京100083;2.北京林业大学省部共建森林培育与保护教育部重点实验室,北京100083
  • 收稿日期:2006-04-25 修回日期:1900-01-01 出版日期:2007-10-25 发布日期:2007-10-25

Soil Water Characteristics of Mixed Coniferous and Deciduous Forest in Low Mountain Area in Beijing

Nie Lishui1,Li Jiyue2,Dai Wei1   

  1. 1. College of Soil and Water Conservation,Beijing Forestry University Beijing 100083; 2. Key Lab.for Silviculture and Conservation of Ministry of Education,Beijing Forestry University Beijing 100083
  • Received:2006-04-25 Revised:1900-01-01 Online:2007-10-25 Published:2007-10-25

摘要: 探讨林地土壤物理性质、土壤含水量的动态变化与土壤水分有效性的关系。研究表明:林地土壤密度为1.20~1.45Mg·m-3,总孔隙度为45%~58%,非毛管孔隙度为6%~10%,通气性略差。应用压力膜仪测定和拟合土壤水分特征曲线符合Gardner提出的经验方程θv=ΑS-B。林地土层厚80cm,土壤总持水量为418.77mm,土壤的田间持水量为348.53mm,土壤在凋萎湿度时的持水量为34.01mm。土壤有效水范围为土壤的田间持水量与土壤的凋萎湿度持水量之差,为314.52mm。土壤贮水量变化在60~180mm,远远低于土壤的田间持水量。从4月下旬到6月上旬土壤的平均容积含水量为最小,土壤平均容积含水量接近10%,为土壤的旱季;土壤在7月至9月上旬为最高含水量时期,土壤平均容积含水量为15%~20%。其他时段的土壤平均容积含水量在10%~15%。

关键词: 土壤物理性质, 土壤水分特征曲线, 土壤凋萎湿度, 土壤含水量

Abstract: This research was aimed to study the soil physical properties,the soil water characteristics and their influences on the plant available soil water in a mixed forest of Pinus tabulaeformis and Quercus variabilis in the Xishan Mountain.The soil had good physical properties as follows:soil density is 1.20~1.45 Mg·m-3,total porosity,45%~58% while the non-capillary porosity,6%~10%,and the root is in poor aeration.The soil moisture characteristic curve could be described by the Gardner empirical equation θv=ΑS-B.The soil had a water holding capacity of 418.77 mm while the field water holding capacity was 348.53 mm and the soil wilting capacity 34.01 mm.So the soil had a field water holding capacity of 314.52 mm.But on site study it was showed the actual water holding capacity never reached such high level.The actual water storage was 60~180 mm,much lower than the field water holding capacity.There existed an about 50 days dry period from late of April to the early of June with the soil moisture lower or near 10%.There existed a humid period from July to early of September with a soil moisture between 15% and 20%.In other period the soil moisture was 10%~15%.

Key words: soil physical properties, soil moisture characteristic curve, soil wilting capacity, soil storage