首页> 外文期刊>Geoderma: An International Journal of Soil Science >Photosynthate-C-13 allocation in the plant-soil system after C-13-pulse labeling of Phragmites australis in different salt marshes
【24h】

Photosynthate-C-13 allocation in the plant-soil system after C-13-pulse labeling of Phragmites australis in different salt marshes

机译:在不同盐沼的C-13脉冲标记后C-13脉冲标记后的植物土系统中的光合素-C-13分配

获取原文
获取原文并翻译 | 示例
           

摘要

Photosynthetic carbon is an integral part of carbon cycle in plant-soil system, also is an important source of soil organic carbon. In this study, C-13 labeling was used for exploring allocation of photosynthate-C-13 in Phragmites australis -soil system undergoing the salt marsh restoration project by freshwater pumping in Yellow River Estuary (YRE), China. Samples were collected from T-0 (before labeling) to 90 days after labeling (T-4), in natural salt marsh, 5-, 10- and 15-year freshwater pumping areas, respectively. The photosynthate-C-13 contents of soil were gradually decreased to 0 mg/g at T-4 in most areas, while it was 2.21 mg/g in 15-year pumping area, higher than other areas at the last sampling time (T-4). And the allocation of photosynthate-C-13 in soil was increased from 3.58% at T-2 to 44.46% at T-3 in natural salt marsh, while no significant change was found in other areas from T-2 to T-3, followed by the significantly higher photosynthate-C-13 proportion in soils of 15-year pumping area at T-4. EC (R-2 = 0.5972) and small macro-aggregates proportion of soil (R-2 = 0.4829) had positive correlations with A photosynthate-C-13 (the value of photosynthate-C-13 in underground part minus that in soil); silt and clay fractions proportion of soil (R-2 = 0.7044) had negative correlation with Delta photosynthate-C-13. Distribution and transportation of photosynthetic carbon in the underground were affected by soil physical and chemical properties.
机译:光合碳是植物土系统中碳循环的一个组成部分,也是土壤有机碳的重要来源。在该研究中,C-13标记用于通过淡水泵浦在黄河口(Yre),探讨澳大利亚澳大利亚芦苇芦苇系统的光合素-C-13分配。在标记(T-4),在天然盐沼,5-,10-和15年淡水泵浦区域中,从T-0(在标记之前)至90天收集样品。在大多数领域,光合酸酯-C-13土壤的含量逐渐降低至0mg / g,而15年的抽水区是2.21mg / g,比上次采样时间的其他区域高(T -4)。在天然盐沼的T-3的土壤中的光合酸酯-C-13分配从T-3的3.58%增加到44.46%,而T-2至T-3的其他区域没有发现显着变化,其次是T-4的15年泵区土壤中的光合素-C-13比例明显较高。 EC(R-2 = 0.5972)和小型宏观聚集体的土壤(R-2 = 0.4829)与光环酸酯-C-13具有阳性相关性(在土壤中的地下部分中的光合作用-C-13的值) ;淤泥和粘土分数比例的土壤(R-2 = 0.7044)与Delta光合酸酯-C-13具有负相关性。地下光合碳的分布和运输受土壤物理和化学性质的影响。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号