首页|大兴安岭干旱阳坡各退化类型土壤与空气温湿度变化研究

大兴安岭干旱阳坡各退化类型土壤与空气温湿度变化研究

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采用土壤和空气自动记录仪,对大兴安岭干旱阳坡的灌草丛和蒙古栎林以及阴坡的土壤温湿度和空气温湿度进行了测定。结果表明,土壤温度表现为草丛>灌草丛>蒙古栎林>阴坡,其中草丛生长季平均值比阴坡高6.01度,土壤含水量与土壤温度相反,表现为阴坡>蒙古栎林>灌草丛>草丛,其中阴坡比草丛高78%;但是三种类型空气温湿度差异均较小,这些表明土壤温湿度的变化是影响干旱阳坡植被恢复的重要因素。
Changes of Soil and Temperature and Humidity of Air among Various Types of Degradation in Daxing’an Mountains
Scrub and Quercus mongolica in south-facing slope and temperature and humidity of soil and air in north-facing slope in Daxing’an Mountains were determined by adopting soil and air automatic recorder.Result shows that the descending order of soil temperature is grass > bush-grass > Quercus mongolica forest > north-facing slope;average value of growing season in hassock is 6.01 degrees higher than that of the north-facing slope;the soil mois-ture is opposite to the soil temperature,which shows that the north-facing slope > Quercus mongolica forest >bush-grass> hassock,among of which north-facing slope is 78% higher than that of hassock;the difference of three kinds of temperature and humidity of air is small,these show that the change of temperature and humidity of soil are the important factors influencing the vegetation restoration of dry south-facing slope.

Daxing’an Mountainsdry south-facing slopenorth-facing slopesoilairtemperature and humidity

杨菲、王峰、孙海龙、陈冰

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大兴安岭地区营林局,黑龙江 大兴安岭 165000

大兴安岭地区农林科学院,黑龙江 大兴安岭 165000

东北林业大学林学院,黑龙江 哈尔滨 150040

大兴安岭 干旱阳坡 阴坡 土壤 空气 温湿度

重度退化生态系统恢复与重建关键技术研究与示范

2011BAD08B02-02

2015

防护林科技
黑龙江省森林与环境科学研究院 国家林业局三北防护林建设局 黑龙江省三北林业建设指导站

防护林科技

影响因子:0.264
ISSN:1005-5215
年,卷(期):2015.(12)