期刊文献+

干湿交替对东北温带次生林与落叶松人工林土壤有机碳矿化的影响 被引量:14

Effects of Rewetting on Soil Organic Carbon Mineralization in Temperate Secondary Forest and Larix olgensis Plantation of Northeast China
下载PDF
导出
摘要 在中温带的黑龙江省帽儿山地区,采集次生林和落叶松人工林表层(0-10cm)土壤,进行室内有机碳矿化培养。先在不同温度(5,15,25,35℃)下干土培养3d,然后进行不同水平的增湿处理(土壤含水率为25%,50%,75%,100%)继续培养11d。结果表明:加水增湿后两林分土壤有机碳矿化速率均被激发并在短时间(1~4d)内达到最大值,不同处理次生林土壤有机碳矿化速率最大值变化范围为15.94~212.65μg CO2-C/(g.d),落叶松人工林土壤为16.75~110.85μg CO2-C/(g.d)。两林分土壤有机碳矿化速率和矿化量随处理湿度的增加而增大,但落叶松人工林100%湿度处理在培养温度超过5℃时,土壤有机碳矿化速率和矿化量却低于75%湿度处理。高温(≥25℃)和高湿(50%~100%)条件下次生林土壤有机碳矿化的激发效应明显大于落叶松人工林土壤,而且次生林土壤有机碳矿化的湿度敏感性系数(k)和温度敏感性系数(Q10)均大于落叶松人工林土壤。这表明随着温度的升高,干湿交替可导致次生林土壤较落叶松人工林土壤损失更多的碳。 With incubation test,this paper studied the responses of mineralization rate and cumulative mineralized amount of surface soil (0-10 cm) organic carbon to temperature (5,15,25,35℃) and soil rewetting with different moisture (water content: 25%,50%,75%,100%) from secondary forest and Larix olgensis plantation in Maoershan mountain of Heilongjiang province.The results showed that soil organic carbon mineralization (SOCM) rates excited rapidly and reached the maximum in few days (1~4 d) following rewetting treatment.The highest SOCM ates changed from 15.94μg CO2-C/(g·d) to 212.65 μg CO2-C/(g·d) in secondary forest,and from 16.75μg CO2-C/(g·d) to 110.85 μg CO2-C/(g·d) in Larix olgensis plantation.With the increase of water addition,SOCM rates increased,both of secondary forest and Larix olgensis plantation.But when temperature exceeded 5℃,SOCM rates of 100% water treatment were less than 75% water treatment in Larix olgensis plantation.At high temperature (≥ 25℃) and big moisture (50% to 100%) conditions,the rates of SOCM increased in secondary forest were significantly larger than Larix olgensis plantation.In addition,moisture sensitivity coefficients (k) and temperature sensitivity coefficients (Q10) of SOCM in secondary forest were greater than Larix olgensis plantation.This suggested that with the temperature rising,rewetting may lead more organic carbon lost in secondary forest soil than Larix olgensis plantation.
出处 《水土保持学报》 CSCD 北大核心 2010年第5期213-217,222,共6页 Journal of Soil and Water Conservation
基金 国家自然科学基金项目(30671678)
关键词 干湿交替 有机碳矿化 土壤温度 土壤湿度 rewetting organic carbon mineralization soil temperature soil moisture
  • 相关文献

参考文献18

  • 1吴建国,张小全,徐德应.六盘山林区几种土地利用方式对土壤有机碳矿化影响的比较[J].植物生态学报,2004,28(4):530-538. 被引量:73
  • 2汪业勖,赵士洞,牛栋.陆地土壤碳循环的研究动态[J].生态学杂志,1999,18(5):29-35. 被引量:119
  • 3Davidson E A, Janssens I A. Temperature sensitivity of soil carbon decomposition and feedbacks to climate change[J]. Nature,2006, 440(7081) : 165-173.
  • 4Rey A, Petsikos C, Jarvis P G, et al. Effect of temperature and moisture on rates of carbon mineralization in a Mediterranean oak forest soil under controlled and field conditions[J].European Journal of Soil Science,2005, 56(5) : 589-599.
  • 5Leir6s M C, Trasar-Cepeda C, Seoane S, et al. Dependence of mineralization of soil organic matter on temperature and moisture[J]. Soil Biology and Biochemistry, 1999, 31(3) : 327-335.
  • 6Fang C, Moncrieff J B. The dependence of soil CO2 efflux on temperature[J]. Soil Biology and Biochemistry,2001, 33(2) : 155-165.
  • 7杨玉盛,陈光水,董彬,王小国,谢锦升,李灵,卢豪良.格氏栲天然林和人工林土壤呼吸对干湿交替的响应[J].生态学报,2004,24(5):953-958. 被引量:65
  • 8Fierer N, Schimel J P. A Proposed Mechanism for the Pulse in Carbon Dioxide Production Commonly Observed Following the Rapid Rewetting of a Dry Soil[J]. Soil Science Society of America Journal,2003, 67(3): 798-805.
  • 9Wu J, Brookes P C. The proportional mineralization of microbial biomass and organic matter caused by air-drying and rew- etting of a grassland soil[J].Soil Biology and Biochemistry, 2005, 37(:]), 507-515.
  • 10Mclntyre R E S, Adams M A, Ford D J, et al. Rewetting and litter addition influence mineralization and microbial communities in soils from a semi-arid intermittent stream[J]. Soil Biology and Biochemistry, 2009, 41(1) : 92-101.

二级参考文献140

共引文献631

同被引文献367

引证文献14

二级引证文献188

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部