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Human impact on C/N/P accumulation in lake sediments from northeast China during the last 150 years

机译:在过去的150年中,来自东北苏州沉积物中C / N / P积累的人类影响

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摘要

Lakes and lake sediments are significant components of the global carbon (C) cycle, and may store very large amounts of organic matter. Carbon sequestration in lakes is subject to substantial temporal and spatial variation and may be strongly affected by human activities. Here, we report accumulation rates (AR) of organic C (OC), total nitrogen (TN) and total phosphorous (TP), and investigate their responses to anthropogenic impact over the past 150 years by analyzing 62 sediment cores from 11 shallow lakes in the Songnen Plain, northeast China. From the center of each of the lakes, we selected one master core for age determination by Pb-210 and Cs-137 radioisotopes. The contents of OC, TN, TP, dry bulk density and mass specific magnetic susceptibility were then determined for all cores. The regional OCAR, TNAR and TPAR up-scaling from the multiple cores yielded mean values of 51.63 +/- 15.13, 2.50 +/- 0.98, and 0.90 +/- 0.21 g m(-2) yr(-1), respectively. Nutrient AR in the studied lakes increased by a factor of approximately 2 x from the middle 19th century to the 1950s, and approximately 5 x after the 1950s. Elemental ratios show that the increase in OCAR is mainly the result of C autogenesis from the growth of aquatic plants stimulated by agricultural intensification, including increased chemical fertilizer application and farmland expansion. Significantly enhanced nutrient burial by these lakes after the 1950s resulted from increased anthropogenic impacts in northeast China. More sustainable agricultural practises, including a decrease in P fertilizer use, would result in a lowering of OCAR, TNAR and TPAR in the future. (C) 2020 Elsevier Ltd. All rights reserved.
机译:湖泊和湖泊沉积物是全球碳(C)循环的重要组成部分,也可以存储非常大量的有机物。湖泊中的碳封存受到大量时间和空间变异的影响,可能受人类活动的强烈影响。在此,我们报告有机C(OC),总氮(TN)和总磷(TP)的积累速率(AR),并通过分析来自11个浅湖的62个沉积物核心来研究过去150年对人为影响的反应宋嫩平原,中国东北。从每个湖泊的中心,我们选择了一个由PB-210和CS-137放射性机电图的年龄确定的一个主核心。然后确定所有芯的OC,TN,TP,干燥堆积密度和质量特异性磁化率的含量。来自多个核心的区域OCAL,TNAR和TPAR上缩放,分别产生51.63 +/-15.13,2.50 +/- 0.98和0.90 +/- 0.21g m(-2)Yr(-1)的平均值。学习湖中的营养AR在19世纪十世纪至20世纪50年代增加了大约2次,在20世纪50年代之后大约5次。元素比例表明,OCAR的增加主要是C患有农业强化刺激的水生植物生长的结果,包括增加化肥应用和农田扩张。在20世纪50年代之后,这些湖泊显着增强了这些湖泊的营养因素,从而提高了中国东北地区的人为影响。更可持续的农业实践,包括降低P肥料使用,将来会导致未来的OCAL,TNAR和TPAR降低。 (c)2020 elestvier有限公司保留所有权利。

著录项

  • 来源
    《Environmental Pollution》 |2021年第2期|116345.1-116345.11|共11页
  • 作者单位

    South China Normal Univ Sch Geog Sci Guangzhou 510631 Peoples R China;

    Univ Alberta Dept Lab Med & Pathol Edmonton AB T6G 2G3 Canada;

    Univ Verona Dept Biotechnol Str Le Grazie 15 I-37134 Verona Italy;

    East China Normal Univ Sch Geog Sci Shanghai 200241 Peoples R China|Univ Cape Town Dept Environm & Geog Sci ZA-7701 Rondebosch South Africa|Zhejiang Normal Univ Coll Geog & Environm Sci Jinhua 321004 Zhejiang Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Lacustrine sediments; Carbon burial; Nutrient; Agriculture; Fertilizer; Eutrophication; Anthropocene;

    机译:湖泊沉积物;碳埋葬;营养;农业;肥料;富营养化;人类;
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