雷州半岛红树林表层沉积物正构烷烃组成分布特征研究

Composition and distribution of n-alkanes in surface sediments of mangrove of Leizhou peninsula

  • 摘要: 本文研究了雷州半岛高桥镇、特呈岛、湖光镇和金沙湾4个区域红树林表层沉积物中正构烷烃的含量、组成分布及来源特征。结果表明,研究区域红树林表层沉积物中总有机碳(TOC)含量为0.10% ~ 5.62%,正构烷烃总含量(∑n-Alk)为0.69 ~ 16.60 μg/g(dw)。红树林表层沉积物中正构烷烃组成以中长链(n-C23 ~ n-C31)为主,呈单峰型分布。除金沙湾以外,其他区域红树林表层沉积物中正构烷烃组成奇偶优势明显。正构烷烃组成分布及平均链长(ACL)、碳优势指数(CPI)、短链/长链比值(∑n-C20/∑n-C21+)、陆海来源比值(TAR)、水生植物贡献比值(Paq)等指标的主成分分析(PCA)结果显示,研究区域红树林表层沉积物中正构烷烃主要来源于高等植物,其中,高桥镇红树林表层沉积物中正构烷烃主要来源于陆源高等植物,而部分湖光镇、特呈岛红树林表层沉积物中正构烷烃的水生植物来源贡献较大,金沙湾红树林表层沉积物中正构烷烃可能受人类活动的影响。因此,本研究认为,红树林表层沉积物中正构烷烃的组成分布可以较好地反映其物源输入特征。

     

    Abstract: The content, composition distribution, and source characteristics of n-alkanes in the surface sediments from four mangrove forests of Gaoqiao town, Techeng island, Huguang town, and Jinsha bay of Leizhou peninsula are studied. The results show that the content of total organic carbon (TOC) in these mangrove surface sediments is between 0.10% to 5.62%, and the content of total n-alkanes (∑n-Alk) ranges from 0.69 to 16.60 μg/g(dw). The composition of n-alkanes in these surface sediments is dominated by medium to long chains n-alkanes (n-C23 to n-C31), that are distributed as unimodal patterns. The n-alkanes display a clear odd-even predominance with an exception of samples from Jinsha bay. The composition and distribution of n-alkanes and the principal component analysis of related index of average chain length (ACL), carbon predominance index (CPI), short-chain/long-chain ratio (∑n-C20/∑n-C21+), terrigenous/aquatic ratio (TAR), and proxy of aquatic macrophyte input (Paq) shows that the n-alkanes in mangrove sediments is mainly sourced from higher plants, among these the n-alkanes in Gaoqiao town mangrove surface sediments are mainly originated from the terrestrial higher plant, while the aquatic plant sourced contribution in the Techeng island and some samples of Huguang town are higher, and the mangrove surface sediments in Jinsha bay is effected by human activities. Therefore, we believe that the composition and distribution of n-alkanes in mangrove surface sediments could be used to reflect the characteristic of their source inputs.

     

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