1. 黄河交通学院,河南,焦作,454000
2. 河南理工大学,河南,焦作,454000
纸质出版:2022
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王琳, 李娜, 文广超, 等. 黄河流域河南段植被覆盖度变化及其驱动力[J]. 水土保持通报, 2022,42(6):393-399.
Wang Lin, Li Na, Wen Guangchao, et al. Vegetation Coverage Changes and Driving Forces in He’nan Section of Yellow River Basin[J]. Bulletin of Soiland Water Conservation, 2022, 42(6): 393-399.
王琳, 李娜, 文广超, 等. 黄河流域河南段植被覆盖度变化及其驱动力[J]. 水土保持通报, 2022,42(6):393-399. DOI: 10.13961/j.cnki.stbctb.20221017.002.
Wang Lin, Li Na, Wen Guangchao, et al. Vegetation Coverage Changes and Driving Forces in He’nan Section of Yellow River Basin[J]. Bulletin of Soiland Water Conservation, 2022, 42(6): 393-399. DOI: 10.13961/j.cnki.stbctb.20221017.002.
[目的] 探究黄河流域河南段的生态状况,分析该区植被生长发育规律及其主控因素,为该区乃至整个黄河流域生态保护和恢复提供理论依据和技术支持。 [方法] 以黄河流域河南段为研究区,利用2001-2020年MODIS-NDVI影像,选取气象、地形、土地利用类型等因素,采用像元二分模型、一元线性回归方程和地理探测器等方法开展黄河流域河南段植被覆盖度变化及其驱动力的研究。 [结果] ①20 a间黄河流域河南段多年平均植被覆盖度由0.54增长到0.71,年增长率为0.85%,中等植被覆盖度(0.45<FVC≤0.6)、中低植被覆盖度(0.3<FVC≤0.45)、低植被覆盖度(0.1<FVC≤0.3)、裸地(FVC≤0.1)向中高植被覆盖度(0.6<FVC≤0.75)、高植被覆盖度(FVC≥0.75)转化,等级面积分别增加12.60%,75.49%; ②空间上,高、中高植被覆盖度区域主要集中在西部伏牛山、北部太行山山区和东部平原区,中等、中低、低植被覆盖度区域主要集中在中部洛阳至郑州段,裸地主要分布在水系和黄河两岸; ③20 a间研究区植被覆盖度改善面积远大于退化面积,极显著改善区域面积比例31.11%,主要分布在西部伏牛山和北部太行山山区;显著改善区域面积比例9.42%,主要分布在极显著改善区域周边;未发生明显变化区域比例52.35%;显著退化和极显著退化区域面积比例分别为3.01%和4.11%,主要分布在中部、东部平原的耕地和建筑物区; ④各因子对植被覆盖度的影响表现为:土地利用类型>高程>坡度>降水量>气温,土地利用类型与高程的交互协同作用对植被覆盖度空间格局分布的影响力达到0.52。 [结论] 2001-2020年研究区植被覆盖度呈现显著改善趋势,空间差异性明显,土地利用类型是影响植被覆盖度的主要影响因子。
[Objective] The ecological status of He’nan section of the Yellow River basin
the growth and development of vegetation in the area
and the main factors controlling vegetation coverage were determined in order to provide a theoretical basis and technical support for the ecological protection and restoration of the area and even the entire Yellow River basin. [Methods] We acquired MODIS-NDVI images for the Yellow River basin research area from 2001 to 2020 as well as meteorological
topographic
and land use type data. We used a pixel dichotomy model
univariate linear regression
and a geographic detector to determine changes in vegetation coverage and its driving forces in He’nan section of the Yellow River basin. [Results] ① Over the past 20 years
the annual average fractional vegetation coverage (FVC) in He’nan section of the Yellow River basin increased from 0.54 to 0.71
with an annual growth rate of 0.85%. Medium vegetation coverage (0.45<FVC≤0.6)
medium and low vegetation coverage (0.3<FVC≤0.45)
low vegetation coverage (0.1<FVC≤0.3)
bare land (FVC≤0.1) changed to medium and high vegetation coverage (0.6<FVC≤0.75) and high vegetation coverage (FVC≥0.75)
and the grade area increased by 12.60% and 75.49% respectively. ② Spatially
the areas with high and medium-high vegetation coverage were mainly concentrated in the Funiu Mountains in the west
the Taihang Mountains in the north
and the eastern plain. The areas with medium
medium-low
and low vegetation coverage were mainly concentrated in the central section from Luoyang to Zhengzhou City. The bare land was mainly located in the water system and both banks of the Yellow River. ③ Over the past 20 years
the area of increased vegetation coverage was much larger than the degraded area
and the area of extremely significant improvement accounted for 31.11%
which was mainly located in the Western Funiu Mountains and the Northern Taihang Mountains. The significantly improved areas accounted for 9.42% of the total area
and were mainly located around the extremely significant improved area. The area with no significant change accounted for 52.35% of the total area. The area of significantly degraded and extremely significantly degraded areas accounted for 3.01% and 4.11%
respectively
of the total area
and were mainly located in the cultivated land and built-up areas of the central and eastern plains. ④ The magnitude of the effects of various factors on vegetation coverage followed the order of land use type > elevation > slope > precipitation > temperature. The interaction and synergy of land use type and elevation had an impact on the spatial pattern distribution of vegetation coverage of 0.52. [Conclusion] Vegetation coverage in the study area significantly increased from 2001 to 2020
with obvious spatial differences. Land use type was the main factor affecting vegetation coverage.
庞家泰,段金亮,张瑞,等.2000-2019年渭河流域植被覆盖度时空演变特征及气候响应[J].水土保持研究,2021,28(5):230-237.
陆荫,张强,李晓红,等.黄河流域甘肃段植被覆盖度时空变化及对气候因子的响应[J].水土保持通报,2020,40(2):232-238.
Wookey P A, Aerts R, Bardgett R D, et al. Ecosystem feedbacks and cascade processes:Understanding their role in the responses of Arctic and alpine ecosystems to environmental change[J]. Global Change Biology, 2010,15(5):1153-1172.
陈耀,张可云,陈晓东,等.黄河流域生态保护和高质量发展[J].区域经济评论,2020(1):8-22.
张志强,刘欢,左其亭,等.2000-2019年黄河流域植被覆盖度时空变化[J].资源科学,2021,43(4):849-858.
李晶,闫星光,闫萧萧,等.基于GEE云平台的黄河流域植被覆盖度时空变化特征[J].煤炭学报,2021,46(5):1439-1450.
贺振,贺俊平.近32年黄河流域植被覆盖时空演化遥感监测[J].农业机械学报,2017,48(2):179-185.
孙高鹏,刘宪锋,王小红,等.2001-2020年黄河流域植被覆盖变化及其影响因素[J].中国沙漠,2021,41(4):205-212.
范彦淳.河南省黄河流域水土保持生态建设成效及做法[J].中国水土保持,2016(10):24-26.
李苗苗,吴炳方,颜长珍,等.密云水库上游植被覆盖度的遥感估算[J].资源科学,2004,26(4):153-159.
赵子娟,范蓓蕾,王玉庭,等.2000-2018年西辽河流域植被覆盖度时空变化特征及影响因素研究[J].中国农业资源与区划,2021,42(12):75-88.
王劲峰,徐成东.地理探测器:原理与展望[J].地理学报,2017,72(1):116-134.
夏兴生,朱秀芳,潘耀忠,等.农作物干旱灾害实时风险监测研究:以2014年河南干旱为例[J].自然灾害学报,2016,25(5):28-36.
刘晓璐,周廷刚,温莉,等.基于VSWI和SPI的2000-2016年河南省干旱特征研究[J].干旱区地理,2018,41(5):984-991.
中华人民共和国水利部. SL 665-2014北方土石山区水土流失综合治理技术标准[S].北京:中国水利水电出版社,2014:1-27.
陈绪钰,李明辉,王德伟,等.采煤诱发地质灾害发育特征与成因机制[J].煤炭技术,2016,35(2):137-139.
金玉玲,耿丽艳,齐庆超.河南矿山环境恢复治理遥感调查与分析[J].矿产保护与利用,2021,41(4):23-27.
王新闯,刘文锴,杨会军,等.河南省植被覆盖度及其景观格局时空变化[J].水土保持通报,2015,35(6):241-247.
刘丽娜,魏杰,马云霞,等.基于时空变化的黄河流域河南段生态环境评价研究[J].环境科学与管理,2021,46(2):169-173.
张静,杜加强,盛芝露,等.1982-2015年黄河流域植被NDVI时空变化及影响因素分析[J].生态环境学报,2021,30(5):929-937.
余玉洋.河南省植被NDVI时空变化及其驱动因子研究[D].河南 开封:河南大学,2018.
颜明,贺莉,王随继,等.基于NDVI的1982-2012年黄河流域多时间尺度植被覆盖变化[J].中国水土保持科学,2018,16(3):86-94.
徐浩杰,杨太保,曾彪.黄河源区植被生长季NDVI时空特征及其对气候变化的响应[J].生态环境学报,2012,21(7):1205-1210.
杨运航,文广超,谢洪波,等.柴达木盆地典型地貌单元归一化植被指数变化特征[J].水土保持通报,2020,40(4):133-139.
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