内蒙古西辽河平原植被指数时空变化及其影响因素研究

高萌萌, 刘琼, 王轶, 李小磊, 石鹏. 内蒙古西辽河平原植被指数时空变化及其影响因素研究[J]. 水文地质工程地质, 2022, 49(1): 175-182. doi: 10.16030/j.cnki.issn.1000-3665.202104046
引用本文: 高萌萌, 刘琼, 王轶, 李小磊, 石鹏. 内蒙古西辽河平原植被指数时空变化及其影响因素研究[J]. 水文地质工程地质, 2022, 49(1): 175-182. doi: 10.16030/j.cnki.issn.1000-3665.202104046
GAO Mengmeng, LIU Qiong, WANG Yi, LI Xiaolei, SHI Peng. Spatial and temporal variations in vegetation index and its impact factors in the West Liaohe Plain in Inner Mongolia[J]. Hydrogeology & Engineering Geology, 2022, 49(1): 175-182. doi: 10.16030/j.cnki.issn.1000-3665.202104046
Citation: GAO Mengmeng, LIU Qiong, WANG Yi, LI Xiaolei, SHI Peng. Spatial and temporal variations in vegetation index and its impact factors in the West Liaohe Plain in Inner Mongolia[J]. Hydrogeology & Engineering Geology, 2022, 49(1): 175-182. doi: 10.16030/j.cnki.issn.1000-3665.202104046

内蒙古西辽河平原植被指数时空变化及其影响因素研究

  • 基金项目: 国家自然科学基金项目(41702386);中国地质调查局地质调查项目(DD20190506;DD20160328);三峡库区地质环境监测与灾害预警重庆市重点实验室开放基金项目(ZD2020A0303);福建省农业生态过程与安全监控重点实验室(福建农林大学)开放基金项目(NYST-2020-02)
详细信息
    作者简介: 高萌萌(1989-),女,硕士,工程师,主要从事生态水文地质研究工作。E-mail:592922470@qq.com
    通讯作者: 刘琼(1986-),女,博士,高级工程师,主要从事环境地质研究工作。E-mail:151796630@qq.com
  • 中图分类号: P641.6

Spatial and temporal variations in vegetation index and its impact factors in the West Liaohe Plain in Inner Mongolia

More Information
  • 西辽河平原位于我国北方农牧交错带,属半干旱气候,发育科尔沁沙地,生态环境极其脆弱,开展植被指数时空变化及其影响因素研究,对于预测土地退化风险意义重大,可为该流域生态环境保护治理及水资源合理开发利用提供技术支撑。利用2000—2019年MODIS NDVI数据,采用一元线性回归趋势法和Mann-Kendall检验分析了近20年来该地区的植被生长变化趋势及突变情况。从影响植被生长的水热条件出发,分析了NDVI值与气象因素(降水、气温)、土壤湿度、地下水埋深等因子的相关关系;结合人类活动,分析了土地利用类型变化对NDVI值的影响。结果表明:(1)2000—2019年生长季NDVI值整体呈上升趋势,不存在显著突变点,最高值0.56,最低值0.41。(2)NDVI值在空间上呈现“东高西低”的分布特征,不同用地类型的NDVI值由大到小依次为耕地>林地>沼泽地>滩地>草地>盐碱地>沙地。(3)92.5%的区域植被呈增长趋势,7.5%的区域植被呈减少趋势。(4)NDVI值与降水、气温、土壤湿度呈正相关关系,相关系数分别为0.86,0.78,0.81,降水对植被影响最大。(5)最适宜天然植被生长的地下水埋深约为3 m,当地下水埋深大于10 m时,NDVI值会随着埋深的增加剧烈减小。(6)人类活动如土地开垦、植树造林是近20年来NDVI值呈增加趋势的主要原因之一,在一定程度上改善了当地生态环境。

  • 加载中
  • 图 1  研究区气象站点和地下水监测站点分布图

    Figure 1. 

    图 2  2000年和2018年研究区土地利用类型分布图

    Figure 2. 

    图 3  研究区2000—2019年NDVI年际变化趋势图

    Figure 3. 

    图 4  研究区NDVI值突变检验曲线图

    Figure 4. 

    图 5  研究区2000—2019年平均NDVI值和植被变化趋势分布图

    Figure 5. 

    图 6  研究区不同土地利用类型NDVI值随季节变化趋势图

    Figure 6. 

    图 7  研究区NDVI值与降水量、气温、表层土壤湿度的相关性分析

    Figure 7. 

    图 8  研究区天然植被NDVI值和地下水埋深关系图

    Figure 8. 

    表 1  研究区2000和2018年土地利用类型面积统计

    Table 1.  Area of different land use types in the study area in 2000 and 2018 /km2

    地类2000年2018年变化
    耕地17 18619 0591 873
    林地217334851312
    草地2406019873−4187
    水域1152569−583
    建设用地13031521218
    滩地306471165
    沙地61997066867
    盐碱地32733053−220
    沼泽地1 9672518551
    裸土地374
    总计57622576220
    下载: 导出CSV
  • [1]

    FOLEY J A, LEVIS S, COSTA M H, et al. Incorporating dynamic vegetation cover within global climate models[J]. Ecological Applications,2000,10(6):1620 − 1632. doi: 10.1890/1051-0761(2000)010[1620:IDVCWG]2.0.CO;2

    [2]

    JIN X M, GUO R H, ZHANG Q, et al. Response of vegetation pattern to different landform and water-table depth in Hailiutu River basin, Northwestern China[J]. Environmental Earth Sciences,2014,71(11):4889 − 4898. doi: 10.1007/s12665-013-2882-1

    [3]

    PAN N Q, FENG X M, FU B J, et al. Increasing global vegetation browning hidden in overall vegetation greening: Insights from time-varying trends[J]. Remote Sensing of Environment,2018,214:59 − 72. doi: 10.1016/j.rse.2018.05.018

    [4]

    BETTS R A. Global vegetation and climate: Self-beneficial effects, climate forcings and climate feedbacks[J]. Journal De Physique IV (Proceedings),2004,121:37 − 60. doi: 10.1051/jp4:2004121002

    [5]

    ZHU L K, SOUTHWORTH J. Disentangling the relationships between net primary production and precipitation in southern Africa savannas using satellite observations from 1982 to 2010[J]. Remote Sensing,2013,5(8):3803 − 3825. doi: 10.3390/rs5083803

    [6]

    刘维, 宋迎波. 2019年秋收作物生长季农业气象条件评价[J]. 中国农业气象,2020,41(3):187 − 190. [LIU Wei, SONG Yingbo. Evaluation of agrometeorological conditions in the growing season of autumn crops in 2019[J]. Chinese Journal of Agrometeorology,2020,41(3):187 − 190. (in Chinese with English abstract) doi: 10.3969/j.issn.1000-6362.2020.03.007

    [7]

    周爱国, 马瑞, 张晨. 中国西北内陆盆地水分垂直循环及其生态学意义[J]. 水科学进展,2005,16(1):127 − 133. [ZHOU Aiguo, MA Rui, ZHANG Chen. Vertical water cycle and its ecological effect in inland basins, Northwest China[J]. Advances in Water Science,2005,16(1):127 − 133. (in Chinese with English abstract) doi: 10.3321/j.issn:1001-6791.2005.01.023

    [8]

    FABRICANTE I, OESTERHELD M, PARUELO J M. Annual and seasonal variation of NDVI explained by current and previous precipitation across Northern Patagonia[J]. Journal of Arid Environments,2009,73(8):745 − 753. doi: 10.1016/j.jaridenv.2009.02.006

    [9]

    KHAN I A A, ARSALAN M H B, SIDDIQUI M F C, et al. Short-term drought assessment in Pakistan and adjoining areas by remote sensing MODIS-NDVI data: A potential consequence of climate change(Article)[J]. Pakistan Journal of Botany,2016,48(5):1887 − 1892.

    [10]

    杨泽元, 王文科, 黄金廷, 等. 陕北风沙滩地区生态安全地下水位埋深研究[J]. 西北农林科技大学学报(自然科学版),2006,34(8):67 − 74. [YANG Zeyuan, WANG Wenke, HUANG Jinting, et al. Research on buried depth of eco-safety about groundwater table in the blown-sand region of the Northern Shaanxi Province[J]. Journal of Northwest Sci-Tech University of Agriculture and Forestry (Natural Science Edition),2006,34(8):67 − 74. (in Chinese with English abstract)

    [11]

    张二勇, 陶正平, 王晓勇, 等. 基于植被结构分析法的生态植被与地下水关系研究—以鄂尔多斯盆地内蒙古能源基地为例[J]. 中国地质,2012,39(3):811 − 817. [ZHANG Eryong, TAO Zhengping, WANG Xiaoyong, et al. A study of vegetation response to groundwater on regional scale in northern Ordos Basin based on structure chart method[J]. Geology in China,2012,39(3):811 − 817. (in Chinese with English abstract) doi: 10.3969/j.issn.1000-3657.2012.03.023

    [12]

    金晓媚, 王松涛, 夏薇. 柴达木盆地植被对气候与地下水变化的响应研究[J]. 水文地质工程地质,2016,43(2):31 − 36. [JIN Xiaomei, WANG Songtao, XIA Wei. Response of vegetation to variation in climate and groundwater in the Qaidam Basin[J]. Hydrogeology & Engineering Geology,2016,43(2):31 − 36. (in Chinese with English abstract)

    [13]

    金晓媚, 张强, 杨春杰. 海流兔河流域植被分布与地形地貌及地下水位关系研究[J]. 地学前缘,2013,20(3):227 − 233. [JIN Xiaomei, ZHANG Qiang, YANG Chunjie. Research on vegetation distribution and its relationship with topography and groundwater depth in the Hailiutu River Basin[J]. Earth Science Frontiers,2013,20(3):227 − 233. (in Chinese with English abstract)

    [14]

    王旭升, 万力, 齐蕊, 等. 鄂尔多斯高原地下水与植被盖度的相互影响[J]. 第四纪研究,2014,34(5):1013 − 1022. [WANG Xusheng, WAN Li, QI Rui, et al. Interactions between groundwater and vegetation coverage in Erdos plateau[J]. Quaternary Sciences,2014,34(5):1013 − 1022. (in Chinese with English abstract) doi: 10.3969/j.issn.1001-7410.2014.05.10

    [15]

    赵捷, 徐宗学, 牛最荣, 等. 黑河上中游流域植被时空演变规律及其对水热条件的响应特征分析[J]. 北京师范大学学报(自然科学版),2016,52(3):387 − 392. [ZHAO Jie, XU Zongxue, NIU Zuirong, et al. Spatiotemporal variation of vegetation in response to changes in temperature and precipitation in upper and middle reaches of the Heihe River basin: a SPOT NDVI dataset study[J]. Journal of Beijing Normal University (Natural Science),2016,52(3):387 − 392. (in Chinese with English abstract)

    [16]

    李元春, 葛静, 侯蒙京, 等. 基于CCI-LC数据的甘南和川西北地区土地覆盖类型时空动态分布及草地面积变化驱动力研究[J]. 草业学报,2020,29(3):1 − 15. [LI Yuanchun, GE Jing, HOU Mengjing, et al. A study of the spatiotemporal dynamic of land cover types and the driving forces of grassland area change in Gannan Prefecture and Northwest Sichuan based on CCI-LC data[J]. Acta Prataculturae Sinica,2020,29(3):1 − 15. (in Chinese with English abstract) doi: 10.11686/cyxb2019263

    [17]

    SPRUCE J P, SADER S, RYAN R E, et al. Assessment of MODIS NDVI time series data products for detecting forest defoliation by Gypsy moth outbreaks[J]. Remote Sensing of Environment,2011,115(2):427 − 437. doi: 10.1016/j.rse.2010.09.013

    [18]

    JIN X M, LIU J T, WANG S T, et al. Vegetation dynamics and their response to groundwater and climate variables in Qaidam Basin, China[J]. International Journal of Remote Sensing,2016,37(3):710 − 728. doi: 10.1080/01431161.2015.1137648

    [19]

    RHIF M, BEN ABBES A, MARTINEZ B, et al. An improved trend vegetation analysis for non-stationary NDVI time series based on wavelet transform[J]. Environmental Science and Pollution Research,2021,28(34):46603 − 46613. doi: 10.1007/s11356-020-10867-0

    [20]

    BIANCHI E, VILLALBA R, SOLARTE A. NDVI spatio-temporal patterns and climatic controls over northern Patagonia[J]. Ecosystems,2020,23(1):84 − 97. doi: 10.1007/s10021-019-00389-3

    [21]

    丁一汇, 张莉. 青藏高原与中国其他地区气候突变时间的比较[J]. 大气科学,2008,32(4):794 − 805. [DING Yihui, ZHANG Li. Intercomparison of the time for climate abrupt change between the Tibetan Plateau and other regions in China[J]. Chinese Journal of Atmospheric Sciences,2008,32(4):794 − 805. (in Chinese with English abstract) doi: 10.3878/j.issn.1006-9895.2008.04.08

    [22]

    刘蓉, 文军, 王欣. 黄河源区蒸散发量时空变化趋势及突变分析[J]. 气候与环境研究,2016,21(5):503 − 511. [LIU Rong, WEN Jun, WANG Xin. Spatial–temporal variation and abrupt analysis of evapotranspiration over the Yellow River source region[J]. Climatic and Environmental Research,2016,21(5):503 − 511. (in Chinese with English abstract)

    [23]

    高彦春, 王金凤, 封志明. 白洋淀流域气温、降水和径流变化特征及其相互响应关系[J]. 中国生态农业学报,2017,25(4):467 − 477. [GAO Yanchun, WANG Jinfeng, FENG Zhiming. Variation trend and response relationship of temperature, precipitation and runoff in Baiyangdian Lake Basin[J]. Chinese Journal of Eco-Agriculture,2017,25(4):467 − 477. (in Chinese with English abstract)

    [24]

    DENG Y H, WANG S J, BAI X Y, et al. Variation trend of global soil moisture and its cause analysis[J]. Ecological Indicators,2020,110:105939. doi: 10.1016/j.ecolind.2019.105939

  • 加载中

(8)

(1)

计量
  • 文章访问数:  977
  • PDF下载数:  7
  • 施引文献:  0
出版历程
收稿日期:  2021-04-15
修回日期:  2021-06-17
刊出日期:  2022-01-15

目录