img

Wechat

  • CN 62-1070/P
  • ISSN 1000-694X
  • Bimonthly 1981
Adv search

Estimation of Aboveground Biomass of Different Degraded Alpine Grassland Based on Vegetation Coverage and Height

  • Lai Chimin ,
  • Lai Riwen ,
  • Xue Xian ,
  • Li Chengyang ,
  • You Quangang ,
  • Huang Cuihua ,
  • Peng Fei
Expand
  • 1. College of Forestry, Fujian Agriculture and Forestry University, Fuzhou 350000, China;
    2. Key Laboratory of Desert and Desertification, Northwest Institute of Ecology and Environmental Resources, Chinese Academy of Sciences, Lanzhou 730000, China;
    3. University of Chinese Academy of Sciences, Beijing 100049, China

Received date: 2018-07-20

  Revised date: 2018-10-18

  Online published: 2019-09-29

Abstract

Due to climate change and irrational human activities, severe degradation of the alpine grassland on the Tibetan Plateau has occurred since the 1980s.Aboveground biomass is one of the most intuitive indicators of grassland degradation. Vegetation coverage and height are commonly used to estimate grassland biomass, but it is unclear whether the relationship between coverage and height and aboveground biomass will maintain after degradation, which affects the accuracy of the estimation of degraded grassland biomass. The relationship between vegetation coverage and height, and the aboveground biomass of alpine meadow and alpine steppe in the central and northeastern Tibetan Plateau under different degraded were studied by multiple regression analysis. Our results show that:(1)aboveground biomass had no significant difference between alpine meadow and alpine steppe (P>0.05) in different degradation stages. (2) As the degree of degradation changes, the effects of vegetation cover and height on aboveground biomass also change. Aboveground biomass was mainly affected by vegetation height in the non-degraded stage and was mainly affected by vegetation coverage after degradation. (3)The aboveground biomass estimated with different models at various degradation stages is closer to the measured value than the biomass estimated by an overall model either in the alpine meadow or alpine steppe. Our results indicate that the estimation of aboveground biomass should be conducted for each degradation level rather than estimating the aboveground biomass using a general model for all levels.

Cite this article

Lai Chimin , Lai Riwen , Xue Xian , Li Chengyang , You Quangang , Huang Cuihua , Peng Fei . Estimation of Aboveground Biomass of Different Degraded Alpine Grassland Based on Vegetation Coverage and Height[J]. Journal of Desert Research, 2019 , 39(5) : 127 -134 . DOI: 10.7522/j.issn.1000-694X.2018.00126

References

[1] 刘伟,周华坤,周立.不同程度退化草地生物量的分布模式[J].中国草地学报,2005,27(2):9-15.
[2] 干友民,成平,周纯兵,等.若尔盖亚高山草甸地上生物量与植被指数关系研究[J].自然资源学报,2009,24(11):1963-1972.
[3] Yang Y H,Fang J Y,Pan Y D,et al.Aboveground biomass in Tibetan grasslands[J].Journal of Arid Environments,2009,73(1):91-95.
[4] 张典业,牛得草,陈鸿洋,等.青藏高原东缘高寒草甸地上生物量的估测模型[J].山地学报,2014,32(4):453-459.
[5] 方金,梁天刚,吕志邦,等.基于高光谱影像的高寒牧区土地覆盖分类与草地生物量监测模型[J].草业科学,2013,30(2):168-177.
[6] 成平.基于TM影像的若尔盖草地退化及生物量模型研究[D].四川:四川农业大学,2009.
[7] 韩波,高艳妮,郭杨,等.三江源区高寒草地地上生物量遥感反演模型研究[J].环境科学研究,2017,30(1):67-74.
[8] 王学霞,董世魁,高清竹,等.青藏高原退化高寒草地土壤氮矿化特征以及影响因素研究[J].草业学报,2018,27(6):1-9.
[9] 卢虎,姚拓,李建宏,等.高寒地区不同退化草地植被和土壤微生物特性及其相关性研究[J].草业学报,2015,24(5):34-43.
[10] 陈乐乐,施建军,王彦龙,等.高寒地区不同退化程度草地群落结构特征研究[J].草地学报,2016,24(1):210-213.
[11] Wang X,Dong S,Yang B,et al.The effects of grassland degradation on plant diversity,primary productivity,and soil fertility in the alpine region of Asia’s headwaters[J].Environmental Monitoring & Assessment,2014,186(10):6903-6917.
[12] 刘纪远,徐新良,邵全琴.近30年来青海三江源地区草地退化的时空特征[J].地理学报,2008,63(4):364-376.
[13] 杜际增,王根绪,李元寿.近45年长江黄河源区高寒草地退化特征及成因分析[J].草业学报,2015,24(6):5-15.
[14] 刘军会,高吉喜,王文杰.青藏高原植被覆盖变化及其与气候变化的关系[J].山地学报,2013,31(2):234-242.
[15] 熊炳桥,赵丽娅,高丹丹.围封对退化沙质草地植物群落的影响[J].中国沙漠,2018,38(2):324-328.
[16] 张镱锂,祁威,周才平,等.青藏高原高寒草地净初级生产力(NPP)时空分异[J].地理学报,2013,68(9):1197-1211.
[17] Barbour M,Burk G,Pitts J H.Terrestrial Plant Ecology[M].London,UK:The Benjamin Publishing Company,1980:222-233.
[18] Xue X,Guo J,Han B S,et al.The effect of climate warming and permafrost thaw on desertification in the Qinghai-Tibetan Plateau[J].Geomorphology,2009,108(3):182-190.
[19] 陈翔,彭飞,尤全刚,等.高寒草甸植被特征对模拟增温的响应——以青藏高原多年冻土区为例[J].草业科学,2016,33(5):825-834.
[20] 徐满厚,刘敏,薛娴,等.增温、刈割对高寒草甸地上植被生长的影响[J].生态环境学报,2015,24(2):231-236.
[21] 姚凤军,齐凤林.退化草地生态系统研究现状[J].畜牧兽医科技信息,2008(11):95-96.
[22] Li N,Wang G,Yang Y,et al.Plant production,and carbon and nitrogen source pools,are strongly intensified by experimental warming in alpine ecosystems in the Qinghai-Tibet Plateau[J].Soil Biology & Biochemistry,2011,43(5):942-953.
[23] 杜小娟.西藏高寒草甸草原生物量异质性研究[D].陕西杨凌:西北农林科技大学,2007.
[24] 尤全刚,薛娴,彭飞,等.高寒草甸草地退化对土壤水热性质的影响及其环境效应[J].中国沙漠,2015,35(5):1183-1192.
[25] 周华坤,赵新全,周立,等.青藏高原高寒草甸的植被退化与土壤退化特征研究[J].草业学报,2005,14(3):31-40.
[26] 曹广民,龙瑞军.放牧高寒嵩草草甸的稳定性及自我维持机制[J].中国农业气象,2009,30(4):553-559.
[27] 周兴民,王质彬,杜庆.青海植被[M].西宁:青海人民出版社,1987:13-25.
[28] 周华坤,赵新全,温军,等.黄河源区高寒草原的植被退化与土壤退化特征[J].草业学报,2012,21(5):1-11.
[29] 阴倩怡,高婷婷,刘鸿芳,等.草地产草量快速调查技术[J].草业科学,2015,32(3):464-469.
[30] Guo Z G,Liang T G,Liu X Y,et al.A new approach to grassland management for the arid Aletai region in Northern China[J].Rangeland Journal,2006,28(2):97-104.
[31] Jiang Y,Zhang Y,Wu Y,et al.Relationships between aboveground biomass and plant cover at two spatial scales and their determinants in northern Tibetan grasslands[J].Ecology & Evolution,2017,7(19):7954-7964.
[32] Qin X J,Sun J,Wang X D.Plant coverage is more sensitive than species diversity in indicating the dynamics of the above-ground biomass along a precipitation gradient on the Tibetan Plateau[J].Ecological Indicators,2018,84(3):507-514.
[33] Li Y H,Luo T X,L Q.Plant height as a simple predictor of the root to shoot ratio:evidence from alpine grasslands on the Tibetan Plateau[J].Journal of Vegetation Science,2010,19(2):245-252.
[34] 张修玉,许振成,宋巍巍,等.西双版纳紫茎泽兰生物量收获的样方选择与模型[J].草业科学,2010,27(10):85-90.
[35] 胡静,侯向阳,萨茹拉,等.基于构件特征的内蒙古典型草原植物羊草个体地上生物量估算[J].草业学报,2015,24(8):211-217.
[36] 童新风,杨红玲,李玉霖,等.科尔沁沙地优势固沙灌木的生物量预测模型[J].中国沙漠,2018,38(3):553-559.
[37] 王蕾,张宏,哈斯,等.基于冠幅直径和植株高度的灌木地上生物量估测方法研究[J].北京师范大学学报(自然科学版),2004,40(5):700-704.
[38] 黎燕琼,郑绍伟,龚固堂,等.不同年龄柏木混交林下主要灌木黄荆生物量及分配格局[J].生态学报,2010,30(11):2809-2818.
[39] 徐满厚,刘敏,翟大彤,等.青藏高原高寒草甸生物量动态变化及与环境因子的关系——基于模拟增温实验[J].生态学报,2016,36(18):5759-5767.
[40] 赵丽娅,高丹丹,熊炳桥,等.科尔沁沙地恢复演替进程中群落物种多样性与地上生物量的关系[J].生态学报,2017,37(12):4108-4117.
Outlines

/