首页> 外文期刊>Agroforestry Systems >Soil carbon and tree litter dynamics in a red cedar–scotch pine shelterbelt
【24h】

Soil carbon and tree litter dynamics in a red cedar–scotch pine shelterbelt

机译:红雪松松树防护林中土壤碳和树木凋落物的动态

获取原文
获取原文并翻译 | 示例
           

摘要

Carbon sequestration in the woody biomass of shelterbelts has been investigated but there have been no measurements of the C stocks in soil and tree litter under this agroforestry practice. The objective of this study was to quantify C stored in surface soil layers and tree litter within and adjacent to a 35-year-old shelterbelt in eastern Nebraska, USA. The 2-row shelterbelt was composed of eastern red cedar (Juniperus virginiana) and scotch pine (Pinus sylvestris). A sampling grid was established across a section of the shelterbelt on Tomek silt loam (fine, smectitic, mesic Pachic Argiudolls). Four soil cores were collected at each grid point, divided into 0–7.5 and 7.5–15 cm depth increments, and composited by depth. Soil samples were analyzed for total, organic, and inorganic C, total N, texture, pH, and nutrient content. Under the shelterbelt, all surface litter in a 0.5 × 0.5 m2 area at each grid point was collected prior to soil sampling, dried, weighed, sorted, and analyzed for total C and N. Average soil organic carbon (SOC) in the 0–15 cm layer within the shelterbelt (3,994 g m?2) was significantly greater than in the cultivated fields (3,623 g m?2). The tree litter contained an additional ~1,300 g C m?2. Patterns of litter mass and soil pH and texture suggested increased organic inputs by tree litter and deposition of wind-blown sediment may be responsible for greater SOC beneath the shelterbelt. Further research is needed to identify the mechanism(s) responsible for the observed patterns of SOC within and adjacent to the shelterbelt and to quantify the C in biomass and deeper soil layers.
机译:已经研究了防护林带木质生物量中的碳固存,但是在这种农林业实践下,尚未测量土壤和树木凋落物中的碳库。这项研究的目的是量化存储在美国内布拉斯加州东部一个35岁的防护林带内和附近的地表土壤层和枯枝落叶中的碳。 2行防护林带由东部红柏(Juniperus virginiana)和苏格兰松(Pinus sylvestris)组成。在托梅克粉砂质壤土(精细,近土性,中性的Pachic Argiudolls)上的防护林的一部分上建立了采样网格。在每个网格点收集了四个土壤核心,分为0-7.5和7.5-15 cm的深度增量,并按深度进行合成。分析土壤样品的总碳,有机碳和无机碳,总氮,质地,pH和养分含量。在防护林带下,在取样土壤之前,收集每个网格点0.5×0.5 m2 区域的所有表面凋落物,干燥,称重,分类并分析总碳和氮。平均土壤有机碳(SOC)防护林带内0–15 cm层中的(3,994 gm?2 )明显大于耕地(3,623 gm?2 )。树木枯枝落叶还含有约1300 g C m?2 。凋落物质量和土壤pH值和质地的模式表明,树木凋落物增加的有机物投入和风吹沉积物的沉积可能是造成防护林下有机碳含量增加的原因。需要进一步的研究来确定造成防护林带内和附近的SOC模式的机制,并量化生物量和深层土壤中的碳。

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