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亚热带毛竹林土壤热通量变异特征
  • ISSN号:0564-3929
  • 期刊名称:《土壤学报》
  • 时间:0
  • 分类:S714.5[农业科学—林学]
  • 作者机构:[1]浙江农林大学浙江省森林生态系统碳循环与固碳减排重点实验室,杭州311300, [2]南京大学国际地球系统科学研究所,南京210093
  • 相关基金:国家自然科学基金重大项目(61190114)、国家“973”重点基础研究发展规划项目(2011CB302705,2010CB950702、2010CB428503)、国家自然科学基金项目(41171324)和浙江农林大学科研发展基金面上项目(2012FK032)资助
中文摘要:

选取2010年12月1日—2011年11月30日的土壤热通量实测数据,通过研究,分析了亚热带(浙江省)毛竹林土壤热通量与三层土壤温度、三层土壤含水量以及净辐射的关系。结果表明:土壤热通量有明显的季节变化特征,而日变化均为“S”形,有一个峰值和一个谷值,月均值差异较明显。年尺度上土壤是热源,土壤热通量为-7.52 MJ m2,占全年净辐射的-0.289%,正向最大值出现在7月(18.71 MJ m2),负向最大值出现在1月(-19.33 MJ m2)。不同时间尺度和不同土壤深度进行回归关系分析,在月尺度上,土壤热通量与土壤5 cm温度的相关性最好,达极显著水平;在日尺度上,土壤热通量与土壤5 cm含水量相关性达极显著水平,但相关系数不高;在月尺度上月均值土壤热通量与净辐射极显著相关,在0.5 h尺度上相关性也为极显著水平,且时间上无延滞现象。

英文摘要:

With its remarkable advantages of rapid growth, high yield, wide application and good economic returns, Phyllostachys edulis has been one of the most extensively cultivated bamboo in China, especially in South China. Soil heat fluxes and meteorological factors of P. edulis ecosystems in Anji were monitored with soil heat flux plates (HFP01) and a meteorological monitoring system. Presently, few works are available on soil heat fluxes in P. edulis ecosystems, but soil heat flux is an important part of ecosystem energy flow. Based on the soil heat flux data measured from Dec. 1st 2010 to Nov. 30th 2011, relationships of soil heat flux with soil temperatures and, soil of water contents in three soil layers and net radiation were analyzed. Results show that soil heat flux varied seasonally with monthly mean flux differing sharply between months, and diurnally, displaying an “S” curve, with one peak and one valley. On an annual scale, soil is the source of heat, providing-7.52 MJ m2 a year and contributing, -0.289% to the total net radiation of a year. The maximum positive value appeared in July and the maximum negative one in January. Regression relationship analysis of different temporal scales and different soil depths shows that on a monthly scale, soil heat flux was best related to the soil temperature at 5 cm in soil depth, showing a relationship at the extremely significant level, while on a daily scale, soil heat flux was in an extremely significant relationship with soil water content at 5 cm in soil depth, but the correlation coefficient was not so high. The monthly mean of soil heat fluxes was extremely significantly related with net radiation on a monthly scale and even at a half-an-hour scale, showing no temporal retardation phenomenon.

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期刊信息
  • 《土壤学报》
  • 北大核心期刊(2011版)
  • 主管单位:中国科学院
  • 主办单位:中国土壤学会
  • 主编:史学正
  • 地址:南京市北京东路71号
  • 邮编:210008
  • 邮箱:actapedo@issas.ac.cn
  • 电话:025-86881237
  • 国际标准刊号:ISSN:0564-3929
  • 国内统一刊号:ISSN:32-1119/P
  • 邮发代号:2-560
  • 获奖情况:
  • 2003年荣获“百种中国杰出学术期刊”称号,2002年荣获“第三届华东地区优秀期刊奖”,2002年荣获“第三届中国科协优秀期刊二等奖”
  • 国内外数据库收录:
  • 美国化学文摘(网络版),英国农业与生物科学研究中心文摘,日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版),中国北大核心期刊(2000版)
  • 被引量:40223