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1980—2005年松嫩平原土壤湿度对气候变化的响应

姜丽霞;李帅;纪仰慧;朱海霞;闫平;王萍;王晨轶;韩俊杰   

  1. 黑龙江省气象科学研究所, 哈尔滨 150030
  • 收稿日期:2008-06-11 修回日期:1900-01-01 出版日期:2009-01-20 发布日期:2009-01-20

Responses of soil humidity on Songnen Plain to climate change in 1980-2005.

JIANG Li-xia;LI Shuai;JI Yang-hui;ZHU Hai-xia;YAN Ping;WANG Ping; WANG Chen-yi;HAN Jun-jie   

  1. Heilongjiang Institute of Meteorological Science, Harbin 150030, China
  • Received:2008-06-11 Revised:1900-01-01 Online:2009-01-20 Published:2009-01-20

摘要: 基于松嫩平原16个农业气象站1980—2005年作物生长季的旬土壤湿度、月气温和月降水量观测资料,采用统计分析方法,分析了研究区表层(0~30 cm)土壤湿度的时空变化特征及其对气温、降水量等气候变化的响应.结果表明:1980—2005年间,松嫩平原不同区域作物生长季表层土壤湿度均呈减小趋势,松嫩平原表层土壤存在干旱化趋向,其中,西部和南部地区尤为明显;20世纪90年代以前,研究区表层土壤处于比较湿润阶段,之后土壤湿度持续降低,并发生了偏干现象;研究期间,松嫩平原作物生长季平均气温呈周期性波动上升,每6 a一个周期,期间小幅波动,1992年开始明显上升;生长季降水量的年际变幅较大,存在一个4~5 a的波动周期;研究区作物生长季表层土壤湿度与气温呈极显著负相关关系,与降水量呈极显著正相关关系(P<0.01).气温和降水量是影响松嫩平原作物生长季表层土壤湿度变化的主要气候因素.

关键词: 水分胁迫, 稳定同位素, 小叶杨, 水分来源, 退化

Abstract: Based on the 1980〖KG-*2〗-〖KG-*7〗2005 observation data of ten-day soil humid ity, monthly air temperature, and monthly precipitation during crop growth perio d (from May to September) from 16 agro-meteorological stations on Songnen Plain , the spatiotemporal variation of surface soil (0〖KG-*2〗-〖KG-*7〗30 cm) humid ity and its responses to the air temperature and precipitation in study area wer e analyzed by using statistical method. The results showed that on Songnen Plain , the surface soil humidity during crop growth period in 1980〖KG-*2〗-〖KG-*7〗 2005 had a decreasing trend, and tended to be aridified, especially in the west and south parts of the Plain. Before the 1990s, the surface soil on the Plain was r elatively humid, but thereafter, the humidity kept decreasing, and partial dryne ss occurred. In the study period, the mean air temperature during crop growth pe riod had a periodical increase before 1992, with a small fluctuation in a cycle of 6 years, but increased obviously after then. The precipitation during crop gr owth period had a larger inter-annual variation, with a cycle of 4〖KG-*2〗-〖K G-*7〗5 years. The surface soil humidity during crop growth period was significa ntly negatively correlated to air temperature and positively correlated to preci pitation. Both air temperature and precipitation were the main climatic factors affecting the variation of surface soil humidity on Songnen Pl ain.

Key words: stable isotope, water source, water stress., degeneration, Populus simonii