[Objectives]To explore the distribution characteristics of soil organic carbon in degraded forest land in the sandstorm area of Jingbian County,Shaanxi Province.[Methods]The distribution characteristics and abundance ...[Objectives]To explore the distribution characteristics of soil organic carbon in degraded forest land in the sandstorm area of Jingbian County,Shaanxi Province.[Methods]The distribution characteristics and abundance of 0-20 cm shallow soil organic carbon in 5 towns in the sandstorm area in the north of Jingbian County were studied by field sampling and indoor detection.[Results]The average soil organic carbon contents in Hongdunjie Town,Haizetan Town,Huanghaojie Town,Ningtiaoliang Town and Dongkeng Town were 2.93,3.21,2.53,2.54 and 4.08 g/kg,respectively,which were all lower than the national background value(31.00 g/kg).The coefficients of variation of soil organic carbon content in Hongdunjie Town,Huanghaojie Town and Dongkeng Town were 59.04%,35.97%and 47.55%,respectively,with higher coefficients of variation and larger differences in spatial distribution.The organic carbon content of Haizetan Town and Dongkeng Town was above the abundance,accounting for 70%and 50%,which were relatively rich,while the soil organic carbon content of Hongdunjie was relatively scarce.The average content of soil organic carbon in the sandstorm area was 3.03 g/kg,which was also lower than the national background value.The coefficient of variation was 46.53%,showing high coefficient of variation and large difference in spatial distribution.In addition,20.41%of the average content of soil organic carbon in the sandstorm area was in the deficient level,and 79.59%were in the medium or above level.[Conclusions]The study of distribution characteristics of soil organic carbon in degraded forest land in the sandstorm area of Jingbian County will better serve the precise management of soil resources.展开更多
黄土作为典型的多物源沉积物,粒度分布常呈现多峰分布。端元分析可以从复杂的沉积物粒度中分离出代表不同沉积物源和沉积动力的端元组分,在黄土研究中得到了广泛应用。利用Paterson参数化端元模型对处于毛乌素沙漠东南缘的靖边三道沟剖...黄土作为典型的多物源沉积物,粒度分布常呈现多峰分布。端元分析可以从复杂的沉积物粒度中分离出代表不同沉积物源和沉积动力的端元组分,在黄土研究中得到了广泛应用。利用Paterson参数化端元模型对处于毛乌素沙漠东南缘的靖边三道沟剖面粒度进行端元分离与解释,并讨论其代表的环境意义。靖边三道沟黄土可分为4个端元:EM1(众数粒径8.93μm)为背景粉尘;EM2(众数粒径25.18μm)为与季风环流有关的组分;EM3(众数粒径39.91μm)和EM4(众数粒径56.37μm)都是与冬季风有关的组分,其中EM3为黄土高原黄土主要组分,EM4与现代沙尘暴的粒级大致相同。通过对各端元组分随年龄变化的曲线进行分析,得到以下结论:该剖面记录了靖边地区自MIS 3以来经历了MIS 3(32.8~29.8 ka BP)、LGM(29.8~22.8 ka BP)、冰消期(22.8~11.3 ka BP)和全新世(8.7~1.7 ka BP)共4个气候时期。端元组分还记录了冰消期H 1事件(16.2~13.8 ka BP)、B/A事件(13.8~12.8 ka BP)、YD事件(12.8~11.3 ka BP)共3次气候快速变化事件和D-O旋回。该剖面还记录了毛乌素沙漠末次冰期经历的3次主要的扩张-收缩旋回以及全新世8.7~8.2,6.0~5.0,3.5~2.5 ka共3次干旱沙进事件。展开更多
基金Supported by the Scientific Research Project of Shaanxi Provincial Land Engineering Construction Group(DJNY2022-21)Shaanxi Province Youth Talent Promotion Program(YKJ202228).
文摘[Objectives]To explore the distribution characteristics of soil organic carbon in degraded forest land in the sandstorm area of Jingbian County,Shaanxi Province.[Methods]The distribution characteristics and abundance of 0-20 cm shallow soil organic carbon in 5 towns in the sandstorm area in the north of Jingbian County were studied by field sampling and indoor detection.[Results]The average soil organic carbon contents in Hongdunjie Town,Haizetan Town,Huanghaojie Town,Ningtiaoliang Town and Dongkeng Town were 2.93,3.21,2.53,2.54 and 4.08 g/kg,respectively,which were all lower than the national background value(31.00 g/kg).The coefficients of variation of soil organic carbon content in Hongdunjie Town,Huanghaojie Town and Dongkeng Town were 59.04%,35.97%and 47.55%,respectively,with higher coefficients of variation and larger differences in spatial distribution.The organic carbon content of Haizetan Town and Dongkeng Town was above the abundance,accounting for 70%and 50%,which were relatively rich,while the soil organic carbon content of Hongdunjie was relatively scarce.The average content of soil organic carbon in the sandstorm area was 3.03 g/kg,which was also lower than the national background value.The coefficient of variation was 46.53%,showing high coefficient of variation and large difference in spatial distribution.In addition,20.41%of the average content of soil organic carbon in the sandstorm area was in the deficient level,and 79.59%were in the medium or above level.[Conclusions]The study of distribution characteristics of soil organic carbon in degraded forest land in the sandstorm area of Jingbian County will better serve the precise management of soil resources.
文摘黄土作为典型的多物源沉积物,粒度分布常呈现多峰分布。端元分析可以从复杂的沉积物粒度中分离出代表不同沉积物源和沉积动力的端元组分,在黄土研究中得到了广泛应用。利用Paterson参数化端元模型对处于毛乌素沙漠东南缘的靖边三道沟剖面粒度进行端元分离与解释,并讨论其代表的环境意义。靖边三道沟黄土可分为4个端元:EM1(众数粒径8.93μm)为背景粉尘;EM2(众数粒径25.18μm)为与季风环流有关的组分;EM3(众数粒径39.91μm)和EM4(众数粒径56.37μm)都是与冬季风有关的组分,其中EM3为黄土高原黄土主要组分,EM4与现代沙尘暴的粒级大致相同。通过对各端元组分随年龄变化的曲线进行分析,得到以下结论:该剖面记录了靖边地区自MIS 3以来经历了MIS 3(32.8~29.8 ka BP)、LGM(29.8~22.8 ka BP)、冰消期(22.8~11.3 ka BP)和全新世(8.7~1.7 ka BP)共4个气候时期。端元组分还记录了冰消期H 1事件(16.2~13.8 ka BP)、B/A事件(13.8~12.8 ka BP)、YD事件(12.8~11.3 ka BP)共3次气候快速变化事件和D-O旋回。该剖面还记录了毛乌素沙漠末次冰期经历的3次主要的扩张-收缩旋回以及全新世8.7~8.2,6.0~5.0,3.5~2.5 ka共3次干旱沙进事件。
