小陇山不同林龄锐齿栎林土壤有机碳和全氮积累特征  

Accumulation of soil organic carbon and total nitrogen in Quercus aliena var.acuteserrata forests at different age stages in the Xiaolongshan Mountains,Gansu Province

作　　者：侯浩[1,2] 张宋智 关晋宏[1,2] 杜盛[2] 

机构地区：[1]西北农林科技大学林学院,杨凌712100 [2]中国科学院水利部水土保持研究所,黄土高原土壤侵蚀与旱地农业国家重点实验室,杨凌712100 [3]甘肃省栎类次生林生态系统重点实验室,小陇山林业科学研究所,天水741022

出　　处：《生态学报》2016年第24期8025-8033,共9页Acta Ecologica Sinica

基　　金：中国科学院战略性先导科技专项(XDA05050202)

摘　　要：以甘肃小陇山林区3个林龄阶段(中龄林、近熟林和成熟林)的锐齿栎(Quercus aliena var.acuteserrata)天然次生林为对象,研究了土壤中有机碳和全氮的垂直分布及其积累特征。结果表明:林地土壤有机碳和全氮含量在各龄级土壤剖面中的垂直变化规律一致,表层土壤中含量最高,随着土层深度逐渐降低。1 m土层范围有机碳和全氮密度随着林龄的增加而增加,中龄林、近熟林和成熟林的碳密度分别为122.92、242.21t/hm^2和280.53 t/hm^2,龄组之间差异显著(P<0.05);3个林龄阶段的土壤全氮密度分别为10.37、18.94t/hm^2和24.76 t/hm^2,差异显著(P<0.05)。有机碳和全氮密度在0—20 cm土层中占有很高比重,达37%—56%。土壤有机碳与全氮含量呈极显著的线性正相关(P<0.0001)。土壤有机碳和全氮积累速率随林龄阶段存在差异,在生长旺盛期(中龄林-近熟林)的土壤有机碳(10.84 t hm^(-2)a^(-1))和全氮(0.78 t hm^(-)2a^(-1))的积累速率要大于成熟期(近熟林-成熟林)的土壤有机碳(1.92 t hm^(-2)a^(-1))和全氮(0.29 t hm^(-2)a^(-1))积累速率。It has been reported that soil constitutes the largest carbon pool in terrestrial ecosystems. Soil organic carbon （SOC） in forest ecosystems is considered a major stock of carbon sequestered by vegetation biomass production. Soil total nitrogen （STN） is typically closely coupled with SOC and contributes to ecosystem productivity. Studies on soil carbon and nitrogen in the forests of Northwest China are relatively few. In order to provide a more accurate assessment of the carbon storage and accumulation characteristics in the forests of this region, we investigated the representative natural secondary forests of Quercus aliena var. acuteserrata in the Xiaolongshan Mountains of Gansu Province. These broadleaved forests are typically found at elevations of 1400--1800 m in this area, the western part of the Qinling Mountains. We selected forest stands of Q. aliena var. acuteserrata at three age stages （ mid-aged, pre-mature, and mature） , and three representative plots （30 m × 20 m） were established for each age stage. Soil samples were taken at three points diagonally across the plot using a soil auger （6-cm internal diameter） at depths of 0--10 cm, 10--20 cm, 20--30 cm, 30--50 cm and 50--100 cm. The cored samples from the same depth in each plot were mixed and all samples were then transferred to the laboratory for further analyses. They were air dried and ground to pass through a 0.25-ram sieve prior to the analyses of carbon and nitrogen. In each plot, we also dug a soil profile （ 1 m depth） and sampled undisturbed soil, with two replicates for each soil layer, using a cutting ring （100 m3）. These soil samples were weighed and their moisture was measured to calculate the bulk density of each layer. The SOC content was determined by the potassium dichromate-sulfuric acid oxidation method. STN content was determined using a FOSS-8400 full-automatic Kjeldahl apparatus. Both SOC and STN densities over a forest area were calculated using their contents multiplied by the soil bulk density a

关 键 词：小陇山 锐齿栎天然次生林 土壤有机碳 土壤全氮 

分 类 号：S714.2[农业科学—林学]