阿尔泰山冷杉林下土壤有机碳矿化特征

刘浩宇; 巩晟萱; 王兵; 戴伟; 庞欢; 张毓涛

doi:10.13961/j.cnki.stbctb.2016.01.058

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阿尔泰山冷杉林下土壤有机碳矿化特征

试验研究

- 阿尔泰山冷杉林下土壤有机碳矿化特征
- Mineralization Characteristics of Soil Organic Carbon Under Abies Nephrolepis Forest in Altai Mountains
- 水土保持通报 2016年36卷第1期页码：327-331
- 作者机构：
  
  1. 北京林业大学林学院,北京,100083
  2. 中国林科院森林生态环境与保护研究所,北京,100091
  3. 新疆林科院森林生态研究所,新疆,乌鲁木齐,830063
- 作者简介：
- 基金信息：
  
  中国森林土壤调查、标准规范及数据库构建(2014FY120700).
- DOI：10.13961/j.cnki.stbctb.2016.01.058
  中图分类号：
- 纸质出版：2016
- 稿件说明：
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刘浩宇, 巩晟萱, 王兵, 等. 阿尔泰山冷杉林下土壤有机碳矿化特征[J]. 水土保持通报, 2016,36(1):327-331.

LIU Haoyu, GONG Shengxuan, WANG Bing, et al. Mineralization Characteristics of Soil Organic Carbon Under Abies Nephrolepis Forest in Altai Mountains[J]. Bulletin of Soiland Water Conservation, 2016, 36(1): 327-331.
刘浩宇, 巩晟萱, 王兵, 等. 阿尔泰山冷杉林下土壤有机碳矿化特征[J]. 水土保持通报, 2016,36(1):327-331. DOI： 10.13961/j.cnki.stbctb.2016.01.058.

LIU Haoyu, GONG Shengxuan, WANG Bing, et al. Mineralization Characteristics of Soil Organic Carbon Under Abies Nephrolepis Forest in Altai Mountains[J]. Bulletin of Soiland Water Conservation, 2016, 36(1): 327-331. DOI： 10.13961/j.cnki.stbctb.2016.01.058.

摘要

[目的

]

探讨阿尔泰山天然冷杉混交林不同海拔梯度下土壤有机碳矿化特征

为天然冷杉林土壤有机碳的分解转化过程研究提供理论依据. [方法

]

以新疆布尔津县境内阿尔泰山1 300~1 500

1 500~1 700

1 700~1 900 m这3个海拔梯度的冷杉(Abies nephrolepis)混交林下土壤为研究对象

在研究了土壤有机碳含量特征的基础上

进一步利用双指数模型对有机碳矿化特点进行了探讨. [结果

]

(1) 3个海拔梯度的土壤有机碳含量均表现出随土层加深而降低的趋势

表层富集现象明显

且该趋势不随海拔梯度的变化而变化; (2) 3个海拔梯度的各土层有机碳矿化趋势相似.即矿化初期CO

-C累积量增幅较大

而到了中、后期矿化曲线逐渐趋于平缓

-C累积量增幅减小; (3) 双指数方程可以很好地拟合出冷杉林土壤有机碳的矿化趋势; (4) 土壤有机碳矿化过程进行到100 d时各海拔梯度的各土层活性碳均未被完全分解; (5) 矿化碳与土壤有机碳总量和活性碳含量均达到极显著相关水平. [结论

]

土壤有机碳矿化过程表现出明显随海拔变化的特征.土壤活性碳含量是影响矿化作用的直接因素.

Abstract

[Objective] The research was conducted to analyze the mineralization characteristics of soil organic carbon in Abies nephrolepis forest at different elevations in Altai mountains in order to provide the theoretic basis for the decompose and conversion processe study of soil organic carbon under A.nephrolepis forest. [Method] The soil samples were collected in A.nephrolepis mixed forests at elevation of 1 300~1 500 m

1 500~1 700 m and 1 700~1 900 m in Altai mountains in Burqin County in Xinjiang Uygur Autonomous Region

and soil organic carbon content was analyzed and compared. The mineralization characteristics of soil organic carbon were further explored using double exponential equation. [Results] (1) Soil organic carbon and active carbon content decreased with increasing soil depth in all three elevation gradient

and the surface accumulation was obvious. (2) The trend of mineralization of soil organic carbon at three elevation gradient was similar. The cumulant of CO2-C was bigger at early stage of mineralization. In the middle and late stage

the curve flatten out gradually

the increasing rate of cumulant of CO2-C decreased. (3) The mineralization characteristics of soil organic carbon in A.nephrolepis forest in each layer can be well simulated using double exponential equation. (4) After 100 days of mineralization

the soil activated carbon at each elevation gradient was not still fully decomposed. (5) Mineralized carbon and soil total organic carbon and active carbon content were significantly correlated. [Conclusion] The mineralization process of soil organic carbon obviously varied with elevation

soil active carbon concentration affected mineralization process directly.

关键词

Keywords

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