...
首页> 外文期刊>Plant and Soil >Response of soil respiration to simulated N deposition in a disturbed and a rehabilitated tropical forest in southern China
【24h】

Response of soil respiration to simulated N deposition in a disturbed and a rehabilitated tropical forest in southern China

机译:中国南方热带雨林中土壤呼吸对模拟氮沉降的响应

获取原文
获取原文并翻译 | 示例

摘要

Responses of soil respiration (CO2 emission) to simulated N deposition were studied in a disturbed (reforested forest with previous understory and litter harvesting) and a rehabilitated (reforested forest with no understory and litter harvesting) tropical forest in southern China from October 2005 to September 2006. The objectives of the study were to test the following hypotheses: (1) soil respiration is higher in rehabilitated forest than in disturbed forest; (2) soil respiration in both rehabilitated and disturbed tropical forests is stimulated by N additions; and (3) soil respiration is more sensitive to N addition in disturbed forest than in rehabilitated forest due to relatively low soil nutrient status in the former, resulting from different previous human disturbance. Static chamber and gas chromatography techniques were employed to quantify the soil respiration, following different N treatments (Control, no N addition; Low-N, 5 g N m-2 year-1; Medium-N, 10 g N m-2 year-1), which had been applied continuously for 26 months before the respiration measurement. Results showed that soil respiration exhibited a strong seasonal pattern, with the highest rates observed in the hot and wet growing season (April-September) and the lowest rates in winter (December-February) in both rehabilitated and disturbed forests. Soil respiration rates exhibited significant positive exponential relationship with soil temperature and significant positive linear relationship with soil moisture. Soil respiration was also significantly higher in the rehabilitated forest than in the disturbed forest. Annual mean soil respiration rate in the rehabilitated forest was 20% lower in low-N plots (71+or-4 mg CO2-C m-2 h-1) and 10% lower in medium-N plots (80+or-4 mg CO2-C m-2 h-1) than in the control plots (89+or-5 mg CO2-C m-2 h-1), and the differences between the control and low-N or medium-N treatments were statistically significant. In disturbed forest, annual mean soil respiration rate was 5% lower in low-N plots (63+or-3 mg CO2-C m-2 h-1) and 8% lower in medium-N plots (61+or-3 mg CO2-C m-2 h-1) than in the control plots (66+or-4 mg CO2-C m-2 h-1), but the differences among treatments were not significant. The depressed effects of experimental N deposition occurred mostly in the hot and wet growing season. Our results suggest that response of soil respiration to elevated N deposition in the reforested tropical forests may vary depending on the status of human disturbance..
机译:2005年10月至9月,在中国南部一个受干扰的(已造林并有凋落物收获的重新造林的森林)和一个经过恢复的(未造林和凋落物收获的重新造林的森林)中研究了土壤呼吸(CO2排放)对模拟氮沉降的响应。 2006年。该研究的目的是检验以下假设:(1)恢复林中的土壤呼吸高于动乱森林中的土壤呼吸; (2)氮素的添加促进了恢复和受干扰的热带森林的土壤呼吸; (3)由于先前人类干扰的不同,土壤呼吸中的土壤养分相对较低,因此土壤呼吸对受干扰森林的氮含量比恢复森林更为敏感。在进行不同的氮处理后(对照,不添加氮;低氮,5 g N m-2年-1;中氮,10 g N m-2年),采用静态室和气相色谱技术定量土壤呼吸。 -1),在呼吸测量之前已连续使用26个月。结果表明,土壤呼吸呈现出强烈的季节性模式,在恢复和受干扰的森林中,湿热生长季节(4月至9月)的呼吸速率最高,而冬季(12月至2月)的呼吸速率最低。土壤呼吸速率与土壤温度呈显着正指数关系,与土壤水分呈显着正线性关系。恢复林中的土壤呼吸也显着高于受干扰林。在低氮地块(71+或-4 mg CO2-C m-2 h-1)中,恢复森林的年平均土壤呼吸速率低20%,在中氮地块(80+或-4)中低10%毫克CO2-C m-2 h-1)比对照地块(89+或5毫克CO2-C m-2 h-1)高,而对照与低氮或中氮处理之间的差异为具有统计意义。在受干扰的森林中,低氮地块(63+或-3 mg CO2-C m-2 h-1)的年平均土壤呼吸速率低5%,而中氮地块(61+或-3)的年平均土壤呼吸速率低8%。毫克CO2-C m-2 h-1)(66 +或-4毫克CO2-C m-2 h-1),但处理之间的差异不显着。实验性氮沉积的抑制作用主要发生在炎热和潮湿的生长季节。我们的结果表明,土壤呼吸对重新造林的热带森林中高氮沉积的响应可能因人为干扰的状况而异。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号