Relationship of Oedaleus decorus asiaticus Densities with Soil Moisture and Land Surface Temperature in Inner Mongolia, China

被引:0
|
作者
Du, Bobo [1 ]
Shan, Yanmin [2 ]
Huang, Wenjiang [3 ]
Dong, Yingying [3 ]
Gao, Shujing [1 ]
Yue, Yuchao [2 ]
Guo, Jing [3 ]
Ga, Liwa [2 ]
Zhang, Yan [3 ]
Han, Haibin [1 ]
机构
[1] Chinese Acad Agr Sci, Inst Grassland Res, Hohhot 010010, Peoples R China
[2] Inner Mongolia Forestry & Grassland Pest Control &, Hohhot 010010, Peoples R China
[3] Chinese Acad Sci, Aerosp Informat Res Inst, Key Lab Remote Sensing & Digital Earth, Beijing 100101, Peoples R China
来源
AGRONOMY-BASEL | 2025年 / 15卷 / 04期
基金
中国国家自然科学基金;
关键词
grasshopper; Generalized Additive Models; soil moisture; land surface temperature; Inner Mongolia; GRASSHOPPER POPULATIONS; LOCUST HABITAT; TIME-SERIES; CLIMATE; WEATHER; PLAGUE; DYNAMICS;
D O I
10.3390/agronomy15040998
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Oedaleus decorus asiaticus (O. decorus) is a significant pest in the grasslands of Inner Mongolia, posing considerable challenges to the development of animal husbandry. To understand the key factors influencing the population distribution of O. decorus, field surveys were conducted from 2018 to 2020, during which the population count, growth stage, and location information of O. decorus were recorded. Daily soil moisture (SM) data and daily land surface temperature (LST) data were obtained from the National Tibetan Plateau Data Center, and a Generalized Additive Model (GAM) was constructed. Our findings indicate that the SM (S8) in August of the previous year is the most critical factor, with an F-value of 27.422, followed by the LST (L10) in October of the previous year, the LST (L6) in June of the survey year, the SM (S9) in September of the previous year, the LST (L3) in March of the survey year, and the LST (L5) in May of the survey year, with F-values of 7.848, 7.223, 5.823, 4.919, and 3.547, respectively. S8 and S9 can be regarded as vital indicators for predicting and monitoring the occurrence of O. decorus. However, the contributions of S8 and S9 to O. decorus density differ considerably. S8 is negatively correlated with O. decorus density, while S9 values below 0.29 m3/m3 can promote the growth of O. decorus. A higher LST during early overwintering correlates with increased O. decorus density. During the survey year, LST emerged as the primary factor affecting grasshopper density. Additionally, it plays a more complex role during incubation periods. This study clearly identifies SM and LST as the major factors influencing the occurrence of O. decorus, which will aid in predicting and monitoring its density.
引用
收藏
页数:15
相关论文
共 50 条
  • [31] Spatiotemporal Analysis of Land Use/Cover Patterns and Their Relationship with Land Surface Temperature in Nanjing, China
    Wang, Ruci
    Hou, Hao
    Murayama, Yuji
    Derdouri, Ahmed
    REMOTE SENSING, 2020, 12 (03)
  • [32] Estimating soil moisture and the relationship with crop yield using surface temperature and vegetation index
    Holzman, M. E.
    Rivas, R.
    Piccolo, M. C.
    INTERNATIONAL JOURNAL OF APPLIED EARTH OBSERVATION AND GEOINFORMATION, 2014, 28 : 181 - 192
  • [33] Simultaneous Retrieval of Land Surface Temperature and Soil Moisture Using Multichannel Passive Microwave Data
    Han, Xiao-Jing
    Yao, Na
    Wu, Zihao
    Leng, Pei
    Han, Wenjing
    Chen, Xueyuan
    IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 2024, 62 : 1 - 10
  • [34] INVESTIGATING THE RELATIONSHIP BETWEEN SHALLOW GROUNDWATER, SOIL MOISTURE AND LAND SURFACE TEMPERATURE USING REMOTELY SENSED DATA
    Hamzeh, Saeid
    Mehrabi, Mohammad
    Alavipanah, Seyed Kazem
    Moghadam, Majid Kiavar
    IGARSS 2018 - 2018 IEEE INTERNATIONAL GEOSCIENCE AND REMOTE SENSING SYMPOSIUM, 2018, : 7789 - 7792
  • [35] Biomass and Its Allocation in Relation to Temperature, Precipitation, and Soil Nutrients in Inner Mongolia Grasslands, China
    Kang, Muyi
    Dai, Cheng
    Ji, Wenyao
    Jiang, Yuan
    Yuan, Zhiyou
    Chen, Han Y. H.
    PLOS ONE, 2013, 8 (07):
  • [36] Seasonal variation in soil temperature and moisture of a desert steppe environment: a case study from Xilamuren, Inner Mongolia
    Chang, Yaowen
    Zhang, Ruiqiang
    Hai, Chunxing
    Zhang, Lixing
    ENVIRONMENTAL EARTH SCIENCES, 2021, 80 (07)
  • [37] Seasonal variation in soil temperature and moisture of a desert steppe environment: a case study from Xilamuren, Inner Mongolia
    Yaowen Chang
    Ruiqiang Zhang
    Chunxing Hai
    Lixing Zhang
    Environmental Earth Sciences, 2021, 80
  • [38] Spatial distribution and environmental significance of phytoliths in the surface soil of the Xilingol Grassland in Inner Mongolia, China
    Chong-Xiao Sun
    Hua Su
    Cai-Qing Guo
    Zhi-Wei Liu
    Ya-Meng Li
    Feng Qin
    Hai-Ming Liu
    Palaeobiodiversity and Palaeoenvironments, 2021, 101 : 245 - 258
  • [39] Assessing the relationship between surface temperature and soil moisture in southern Africa
    Pinheiro, AC
    Tucker, CJ
    Entekhabi, D
    Privette, JL
    Berry, JA
    REMOTE SENSING AND HYDROLOGY 2000, 2001, (267): : 296 - 301
  • [40] Land surface temperature assimilation into a soil moisture-temperature model for retrieving farm-scale root zone soil moisture
    Ahmadi, Saeed
    Alizadeh, Hosein
    Mojaradi, Barat
    GEODERMA, 2022, 421