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作 者:张洪文 吕祥熙 孙艳秋 赵建 邵吉亮 王刚[1,2] 韩科胤 闫岩 郑一阳 ZHANG Hong-wen;LYU Xiang-xi;SUN Yan-qiu;ZHAO Jian;SHAO Ji-liang;WANG Gang;HAN Ke-yin;YAN Yan;ZHENG Yi-yang(Mudanjiang Natural Resources Comprehensive Survey Center,Mudanjiang 157021,Heilongjiang Province,China;Hulun Buir Field Scientific Observation and Research Station for Black Earth Key Belt,Hulun Buir 021599,Inner Mongolia,China;Mudanjiang No.2 Senior High School,Mudanjiang 157021,Heilongjiang Province,China)
机构地区:[1]中国地质调查局牡丹江自然资源综合调查中心,黑龙江牡丹江157021 [2]呼伦贝尔黑土地地球关键带野外科学观测研究站,内蒙古呼伦贝尔021599 [3]牡丹江市第二高级中学,黑龙江牡丹江157021
出 处:《地质与资源》2025年第1期11-20,共10页Geology and Resources
基 金:中国地质调查局项目“三江平原宝清湿地退化区1∶5万地表基质调查”(DD20242039);“三江平原桦南-虎林地区黑土地地表基质调查”(ZD20220859);“基于遥感大数据的三江平原黑土区退耕还湿潜力研究”(QCJJ2023-36).
摘 要:对密山黑土剖面(0~1.42 m)开展年代学、磁化率、粒度和元素地球化学研究,结果表明,密山市黑土剖面沉积物以粉砂为主,占比约70%;年龄曲线显示密山市黑土的沉积速率为9.62 cm/ka.元素地球化学数据显示,密山黑土剖面的主要常量元素组合特征与其他典型风成堆积物相似,上部陆壳(UCC)标准化曲线的变化趋势基本一致,表明密山黑土成土母质可能为风成成因.多指标综合分析表明,密山黑土剖面自全新世以来的气候变化经历了3个阶段:早全新世的升温变暖、中全新世的温暖湿润和晚全新世降温变凉.The paper studies the geochronology,magnetic susceptibility,particle size and element geochemistry of black soil profile(0-1.42 m)in Mishan City.The results show that the sediments of black soil profile are mainly silt,accounting for about 70%,and the deposition rate of black soil is 9.62 cm/ka according to the age curve.The element geochemical data reveals that the major element combination characteristics of Mishan black soil profile are similar to those of other typical eolian deposits,and the change trend of UCC-normalized curves is basically the same,indicating the parent material of Mishan black soil may be of aeolian origin.The multi-index comprehensive analysis shows that the climate change of Mishan black soil profile since Holocene has experienced three stages,i.e.temperature rising in the Early Holocene,warm and humid in the Middle Holocene and cooling down in the Late Holocene.
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