海螺沟冰川退缩区不同演替阶段植被碳贮量与分配格局
|
摘要
在贡嘎山海螺沟冰川退缩区的植被演替序列典型地段依次设置8块样地,通过调查生物量,测定含碳率,计算碳贮量,分析演替过程不同阶段各个碳库变化过程,探索原生演替序列碳的动态变化。结果表明:原生演替序列8个样地的碳贮量分别为4.36、51.29、122.08、145.86、169.08、226.55、321.02、346.10 t/hm~2,其中乔木层和土壤层碳贮量在整个演替序列上所占比例均超过85%。土壤所占比例随演替进行持续增加,由S1的21.20%增加到S8的41.86%;乔木所占比例则呈现先增加后减小的趋势,由S1的66.37%下降到S8的52.16%;其余各层在各个阶段所占比例较小。通过对海螺沟冰川退缩区植被演替序列各个阶段植被含碳率和碳贮量的测定,构建了原生演替不同阶段的碳分配和碳贮量格局,对研究原生演替过程中的碳循环以及植被恢复都有积极意义。
Eight sample plots were set in the glacier retreated area of Hailuogou. By investigating biomass,determining the carbon content, calculating carbon storage and analyzing the changes of carbon pools, the carbon dynamic changes of the primary succession sequence was explored. Results show that the carbon storage of 8 plots are 4.36, 51.29, 122.08, 145.86, 169.08, 226.55, 321.02, 346.10 t/hm~2, respectively. Carbon storage in arbor and soil layers account for more than 85% of the whole succession sequence, in which the proportion of soil continue to increase from 21.20% of S1 to 41.86% of S8, while the proportion of arbor increases first and then decreases, from 66.37% of S1 to 52.16% of S8, the proportion of other layers in each stage is small. Through the determination of vegetation carbon content and carbon storage in each stage, the carbon distribution and carbon storage pattern of different stages of primary succession are constructed. This has positive implications for studying the carbon cycle and vegetation restoration in the process of primary succession.
Eight sample plots were set in the glacier retreated area of Hailuogou. By investigating biomass,determining the carbon content, calculating carbon storage and analyzing the changes of carbon pools, the carbon dynamic changes of the primary succession sequence was explored. Results show that the carbon storage of 8 plots are 4.36, 51.29, 122.08, 145.86, 169.08, 226.55, 321.02, 346.10 t/hm~2, respectively. Carbon storage in arbor and soil layers account for more than 85% of the whole succession sequence, in which the proportion of soil continue to increase from 21.20% of S1 to 41.86% of S8, while the proportion of arbor increases first and then decreases, from 66.37% of S1 to 52.16% of S8, the proportion of other layers in each stage is small. Through the determination of vegetation carbon content and carbon storage in each stage, the carbon distribution and carbon storage pattern of different stages of primary succession are constructed. This has positive implications for studying the carbon cycle and vegetation restoration in the process of primary succession.
引文
[1]Walther G R,Post E,Convey P,et al.Ecological responses to recent climate change[J].Nature,2002,416(6879):389-395.
[2]刘纪远,于贵瑞,王绍强,等.陆地生态系统碳循环及其机理研究的地球信息科学方法初探[J].地理研究,2003,22(4):397-405.
[3]Dixon R K,Solomon A M,Brown S,et al.Carbon pools and flux of global forest ecosystems[J].Science,1994,263(5144):185-190.
[4]程鹏飞,王金亮,王雪梅,等.森林生态系统碳储量估算方法研究进展[J].林业调查规划,2009,34(6):39-45.
[5]王金亮,王小花,岳彩荣,等.滇西北香格里拉森林4个建群种的含碳率[J].生态环境学报,2012,21(4):613-619.
[6]曹明奎,于贵瑞,刘纪远,等.陆地生态系统碳循环的多尺度试验观测和跨尺度机理模拟[J].中国科学(D辑:地球科学),2004,34(S2):1-14.
[7]Alexander E B,Burt R.Soil development on moraines of Mendenhall Glacier,southeast Alaska.1.The moraines and soil morphology[J].Geoderma,1996,72(1/2):1-17.
[8]Egli M,Mavris C,Mirabella A,et al.Soil organic matter formation along a chronosequence in the Morteratsch proglacial area(Upper Engadine,Switzerland)[J].Catena,2010,82(2):61-69.
[9]钟祥浩,罗辑,吴宁.贡嘎山森林生态系统研究[M].成都:成都科技大学出版社,1997.
[10]陈富斌,罗辑.贡嘎山高山生态环境研究:第2卷[M].北京:气象出版社,1998.
[11]罗天祥,石培礼,罗辑,等.青藏高原植被样带地上部分生物量的分布格局[J].植物生态学报,2002,26(6):668-676.
[12]刘兴良,马钦彦,杨冬生,等.川西山地主要人工林种群根系生物量与生产力[J].生态学报,2006,26(2):542-551.
[13]李登秋,居为民,郑光,等.基于生态过程模型和森林清查数据的森林生长量估算对比研究[J].生态环境学报,2013,22(10):1647-1657.
[14]张修玉,管东生,张海东.广州三种森林粗死木质残体(CWD)的储量与分解特征[J].生态学报,2009,29(10):5227-5236.
[15]何帆,王得祥,张宋智,等.小陇山林区主要森林群落凋落物及死木质残体储量[J].应用与环境生物学报,2011,17(1):46-50.
[16]周鹏.贡嘎山东坡垂直带谱典型植被类型固碳分异及其影响因子[D].北京:中国科学院大学,2013.
[17]陈有超.贡嘎山东坡峨眉冷杉林碳贮量与碳平衡[D].北京:中国科学院大学,2013.
[18]程根伟,罗辑.贡嘎山亚高山林地碳的积累与耗散特征[J].地理学报,2003,58(2):179-185.
[19]潘辉,黄石德,洪伟,等.3种相思人工林生态系统碳贮量及分配[J].福建林学院学报,2009,29(1):28-32.
[20]杨卫星,李春宁,付军,等.桂西南连续年龄序列尾巨桉人工林碳储量及其分布特征[J].农业研究与应用,2017(3):24-30.
[21]罗辑,李伟,佘佳,等.贡嘎山海螺沟冰川退缩区植被演替过程的碳动态[J].山地学报,2017,35(5):629-635.
[22]周玉荣,于振良,赵士洞.我国主要森林生态系统碳贮量和碳平衡[J].植物生态学报,2000,24(5):518-522.
[23]吕晓涛,唐建维,于贵瑞,等.西双版纳热带季节雨林的C贮量及其分配格局[J].山地学报,2006,24(3):277-283.
[24]涂洁,刘琪璟.亚热带红壤丘陵区湿地松人工林生态系统碳素贮量与分布研究[J].江西农业大学学报,2007,29(1):48-54.
[25]唐宵,黄从德,张健,等.四川主要针叶树种含碳率测定分析[J].四川林业科技,2007,28(2):20-23.
[26]黄从德,张健,杨万勤,等.四川省及重庆地区森林植被碳储量动态[J].生态学报,2008,28(3):966-975.
[27]张萍.北京森林碳储量研究[D].北京:北京林业大学,2009.
[28]马钦彦,陈遐林,王娟,等.华北主要森林类型建群种的含碳率分析[J].北京林业大学学报,2002,24(S1):100-104.
[29]王琪,徐程扬.氮磷对植物光合作用及碳分配的影响[J].山东林业科技,2005,35(5):59-62.
[30]宋蒙亚,余雷,姜永雷,等.贡嘎山冰川退缩迹地植被原生演替驱动机理探究[C]//中国地理学会经济地理专业委员会.2017年中国地理学会经济地理专业委员会学术年会论文摘要集.成都:中国地理学会,2017:38.
[31]杨丹丹,罗辑,佘佳,等.贡嘎山海螺沟冰川退缩区原生演替序列植被生物量动态[J].生态环境学报,2015,24(11):1843-1850.
[32]何磊,唐亚,张继娟,等.原生演替及其在生态恢复中的应用[J].四川师范大学学报(自然科学版),2010,33(3):393-402.
[2]刘纪远,于贵瑞,王绍强,等.陆地生态系统碳循环及其机理研究的地球信息科学方法初探[J].地理研究,2003,22(4):397-405.
[3]Dixon R K,Solomon A M,Brown S,et al.Carbon pools and flux of global forest ecosystems[J].Science,1994,263(5144):185-190.
[4]程鹏飞,王金亮,王雪梅,等.森林生态系统碳储量估算方法研究进展[J].林业调查规划,2009,34(6):39-45.
[5]王金亮,王小花,岳彩荣,等.滇西北香格里拉森林4个建群种的含碳率[J].生态环境学报,2012,21(4):613-619.
[6]曹明奎,于贵瑞,刘纪远,等.陆地生态系统碳循环的多尺度试验观测和跨尺度机理模拟[J].中国科学(D辑:地球科学),2004,34(S2):1-14.
[7]Alexander E B,Burt R.Soil development on moraines of Mendenhall Glacier,southeast Alaska.1.The moraines and soil morphology[J].Geoderma,1996,72(1/2):1-17.
[8]Egli M,Mavris C,Mirabella A,et al.Soil organic matter formation along a chronosequence in the Morteratsch proglacial area(Upper Engadine,Switzerland)[J].Catena,2010,82(2):61-69.
[9]钟祥浩,罗辑,吴宁.贡嘎山森林生态系统研究[M].成都:成都科技大学出版社,1997.
[10]陈富斌,罗辑.贡嘎山高山生态环境研究:第2卷[M].北京:气象出版社,1998.
[11]罗天祥,石培礼,罗辑,等.青藏高原植被样带地上部分生物量的分布格局[J].植物生态学报,2002,26(6):668-676.
[12]刘兴良,马钦彦,杨冬生,等.川西山地主要人工林种群根系生物量与生产力[J].生态学报,2006,26(2):542-551.
[13]李登秋,居为民,郑光,等.基于生态过程模型和森林清查数据的森林生长量估算对比研究[J].生态环境学报,2013,22(10):1647-1657.
[14]张修玉,管东生,张海东.广州三种森林粗死木质残体(CWD)的储量与分解特征[J].生态学报,2009,29(10):5227-5236.
[15]何帆,王得祥,张宋智,等.小陇山林区主要森林群落凋落物及死木质残体储量[J].应用与环境生物学报,2011,17(1):46-50.
[16]周鹏.贡嘎山东坡垂直带谱典型植被类型固碳分异及其影响因子[D].北京:中国科学院大学,2013.
[17]陈有超.贡嘎山东坡峨眉冷杉林碳贮量与碳平衡[D].北京:中国科学院大学,2013.
[18]程根伟,罗辑.贡嘎山亚高山林地碳的积累与耗散特征[J].地理学报,2003,58(2):179-185.
[19]潘辉,黄石德,洪伟,等.3种相思人工林生态系统碳贮量及分配[J].福建林学院学报,2009,29(1):28-32.
[20]杨卫星,李春宁,付军,等.桂西南连续年龄序列尾巨桉人工林碳储量及其分布特征[J].农业研究与应用,2017(3):24-30.
[21]罗辑,李伟,佘佳,等.贡嘎山海螺沟冰川退缩区植被演替过程的碳动态[J].山地学报,2017,35(5):629-635.
[22]周玉荣,于振良,赵士洞.我国主要森林生态系统碳贮量和碳平衡[J].植物生态学报,2000,24(5):518-522.
[23]吕晓涛,唐建维,于贵瑞,等.西双版纳热带季节雨林的C贮量及其分配格局[J].山地学报,2006,24(3):277-283.
[24]涂洁,刘琪璟.亚热带红壤丘陵区湿地松人工林生态系统碳素贮量与分布研究[J].江西农业大学学报,2007,29(1):48-54.
[25]唐宵,黄从德,张健,等.四川主要针叶树种含碳率测定分析[J].四川林业科技,2007,28(2):20-23.
[26]黄从德,张健,杨万勤,等.四川省及重庆地区森林植被碳储量动态[J].生态学报,2008,28(3):966-975.
[27]张萍.北京森林碳储量研究[D].北京:北京林业大学,2009.
[28]马钦彦,陈遐林,王娟,等.华北主要森林类型建群种的含碳率分析[J].北京林业大学学报,2002,24(S1):100-104.
[29]王琪,徐程扬.氮磷对植物光合作用及碳分配的影响[J].山东林业科技,2005,35(5):59-62.
[30]宋蒙亚,余雷,姜永雷,等.贡嘎山冰川退缩迹地植被原生演替驱动机理探究[C]//中国地理学会经济地理专业委员会.2017年中国地理学会经济地理专业委员会学术年会论文摘要集.成都:中国地理学会,2017:38.
[31]杨丹丹,罗辑,佘佳,等.贡嘎山海螺沟冰川退缩区原生演替序列植被生物量动态[J].生态环境学报,2015,24(11):1843-1850.
[32]何磊,唐亚,张继娟,等.原生演替及其在生态恢复中的应用[J].四川师范大学学报(自然科学版),2010,33(3):393-402.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |