首页|兴隆山典型林分土壤呼吸的空间异质性分析

兴隆山典型林分土壤呼吸的空间异质性分析

Spatial heterogeneity analysis of soil respiration in typical forests of the Xinglong Mountains

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为探明兴隆山森林生态系统典型林分土壤碳呼吸的日变化、月际动态特征及其影响因子,利用LI-8100土壤呼吸测定室对辽东栎林、山杨-白桦混交林、油松林和青杄林土壤呼吸速率(Rs)进行连续观测,采用指数方程拟合Rs对土壤温度(T5)、土壤含水量(W5)的响应.结果表明,各林分覆枯落物与裸地的Rs日变化均呈先增加后下降的单峰型曲线,但达到峰值的时间各不相同,各林分Rs与T5间均有显著相关性.各林分Rs在8月达到峰值,为 2.6~7.0 µmol/(m2·s),与其土壤性质的表现一致:辽东栎林和杨桦混交林土壤容重较低,具有较高的全氮、全磷及有机质含量,其Rs亦较高,油松林、青杄林表现相反.枯落物对各林分Rs的贡献率分别为59.83%(辽东栎林)、41.46%(山杨-白桦混交林)、28.68%(油松林)和11.83%(青杄林),各林分覆枯落物时的Rs明显高于裸地.不同林分Rs的变化特征是水热因子联合效应的结果,Rs受T5影响最大,受W5的影响作用相对较小.
Diurnal change,monthly dynamic characteristics and influencing factors of soil respiration in the typical forests of Xinglong Mountains forest ecosystem were identified.The soil respiration rate(Rs)of Quercus wutaishanica forest,Populus davidiana-Betula platyphylla mingled forest,Pinus tabulaefor-mis forest and Picea wilosonii forest were continuously observed by throug the LI-8100 soil respiration measurement room.The exponential equation was used to fit the response of Rs to soil temperature(T5)and humidity(W5).The results showed that the daily variation of Rs of litter and bare land in each stand exhibited a single peak curve of first increasing and then decreasing,but the time to reach the peak was different,and there was a significant correlation between Rs and T5 in each stand.There Rs of each stand all reached the peak in August,with the variation range of 2.6-7.0 µmol/(m2·s).The Rs of each stand in the growth season was consistent with their soil properties:the soil bulk density of Q.wutaishanica for-est and P.davidiana-B.platyphylla mingled forest was low,with high contents of total nitrogen,total phosphorus and organic matter,and their Rs also high.The performance of P.tabulaeformis and P.wiloso-nii was opposite.The contribution rate of litter to Rs in each stand was 59.83%(Q.wutaishanica),41.46%(P.davidiana-B.platyphylla),28.68%(P.wilosonii)and 11.83%(P.tabuliformis)respectively.Rs of each stand covered with litter was significantly higher than that of bare land Rs.The variation charac-teristics of Rs in different stands resulted from the combined effect of water and heat factors,with Rs being most affected by T5,but less affected by W5.

typical forestsoil respiration ratedriver factorXinglong Mountains

凌雷、马成艳、陈徵尼、仲怡铭、王子乔、王翠英

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甘肃兴隆山森林生态系统国家定位观测研究站,兰州 730100

甘肃省林业科学研究院,兰州 730020

典型林分 土壤呼吸速率 驱动因子 兴隆山

2024

兰州大学学报(自然科学版)
兰州大学

兰州大学学报(自然科学版)

CSTPCD北大核心
影响因子:0.855
ISSN:0455-2059
年,卷(期):2024.60(1)