首页|基于SET技术的兴凯湖沼泽湿地表层沉积过程研究

基于SET技术的兴凯湖沼泽湿地表层沉积过程研究

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湿地沉积过程研究对于揭示区域环境演变与湿地发育过程具有重要作用.2011~2015年,在兴凯湖国家级自然保护区,引进并利用地表高程测量仪(surface elevation table,SET),对4处沼泽湿地进行年际尺度表层沉积物累积厚度监测,计算表层沉积物的沉积速率.研究结果表明,2011~2015年期间,4处沼泽湿地表层沉积物的累积厚度分别为(7.31±2.87) mm、(7.70±2.55) mm、(5.71±2.36) mm和(6.30±1.69) mm;表层沉积物的沉积速率分别为(1.85±0.89) mm/a、(2.27±0.91)mm/a、(1.63±0.94) mm/a和(1.45±0.77) mm/a,4处沼泽湿地表层沉积物的沉积速率无显著差异.
Introducing Surface Elevation Table Technique to Monitor Surface Accretion Process in Marshes in Xingkai Lake
Study on the wetland accretion process plays an important role in revealing the regional environmental evolution and wetland development process.This study first introduces surface elevation table (SET) technique to monitor surface accretion depths and calculate the surface accretion rates at 4 sites in the marshes in Xingkai Lake during the years of 2011 and 2015.The results showed that the 4 sites maintained a layer of accreted material (7.31 ±2.87) mm,(7.70±2.55) mm,(5.71±2.36) mm and (6.30± 1.69) mm thickness during the five years of the study,respectively.The 4 sites had average surface accretion rates at (1.85±0.89) mm/yr,(2.27±0.91) mrm/yr,(1.63±0.94) mrm/yr and (1.45±0.77) mm/yr respectively,and there was no significant difference among 4 sites based on the linear regression analyses.This research will provide data and technical support for the high precision study on the accretion process in the inter-annual scale in the marshes in China.

surface sedimentsaccretion ratemarshessurface elevation table (SET)Xingkai Lake

王国栋、吕宪国、刘兴土、姜明

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中国科学院湿地生态与环境重点实验室,中国科学院东北地理与农业生态研究所,吉林长春130102

表层沉积物 沉积速率 沼泽湿地 地表高程测量仪(SET) 兴凯湖

国家林业局重点科技项目国家自然科学基金

2014-0241501105和41620104005

2017

湿地科学
中国科学院 东北地理与农业生态研究所

湿地科学

CSTPCDCSCD北大核心
影响因子:1.52
ISSN:1672-5948
年,卷(期):2017.15(6)
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