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4种植被恢复模式对贵州石漠化地区表层土壤有机碳氮的影响研究

  • 吕文强 ,
  • 唐金刚 ,
  • 罗时琴 ,
  • 林涛 ,
  • 周传艳
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  • 贵州省山地资源研究所,贵阳 550001
吕文强(1982-),男,安徽太和人,助理研究员,主要从事环境地球化学方面的研究工作。Email:lvbuwei123@126.com

收稿日期: 2016-07-02

  修回日期: 2016-09-06

  网络出版日期: 2020-11-02

基金资助

国家自然科学基金(31360123);贵州省科技基金资助项目“喀斯特地区土地利用/覆盖变化对土壤固定碳潜力的影响”(黔科合J字[2014]2114)

Effect of 4 Kinds of Vegetation Restoration Patterns on the Topsoil Organic Carbon and Nitrogen in Rocky Desertification Region of Guizhou Province

  • LÜ Wenqiang ,
  • TANG Jingang ,
  • LUO Shiqin ,
  • LIN Tao ,
  • ZHOU Chuanyan
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  • Institute of Guizhou Mountain Resources,Guiyang 550001,China

Received date: 2016-07-02

  Revised date: 2016-09-06

  Online published: 2020-11-02

摘要

对酥李(Prunus salicina)、核桃(Juglans cathayensis)、石榴(Punica granatum)以及西番莲(Passiflora caerulea)等4种植被治理石漠化模式下土壤有机碳氮含量、密度以及储量进行了研究,结果表明,4种植被恢复模式下:土壤有机碳含量大小顺序为酥李模式>西番莲模式>核桃模式>石榴模式,土壤全氮含量差异较小;0~10cm层土壤有机碳氮含量和密度均大于10~20 cm层;土壤有机碳和全氮储量最高的分别为酥李模式(54.31t/hm2)和西番莲模式(6.21t/hm2);土壤有机碳和全氮储量最低的均为石榴模式,分别为49.77t/hm2和5.66t/hm2。相对而言,酥李模式和西番莲模式是土壤有机碳氮储存能力较高的两种植被恢复模式。

本文引用格式

吕文强 , 唐金刚 , 罗时琴 , 林涛 , 周传艳 . 4种植被恢复模式对贵州石漠化地区表层土壤有机碳氮的影响研究[J]. 林草资源研究, 2016 , 0(5) : 47 -52 . DOI: 10.13466/j.cnki.lyzygl.2016.05.009

Abstract

The topsoil contents,densities and storage of soil organic carbon(SOC) and total nitrogen(TN) of four different vegetation restoration patterns,i.e.,Prunus salicina,Juglans cathayensis,Punica granatum and Passiflora caerulea were studied in rocky desertification region in Guizhou Province.The results showed that the contents of SOC under four different vegetation restoration patterns were in the order of Prunus salicina>Passiflora caerulea>Juglans cathayensis>Punica granatum, while the contents of TN did not differ much.SOC and TN contents and densities in the 0~10 cm soil layer were higer in the 10~20 cm soil layer in each of the four vegetation restoration patterns.SOC storage in the topsoil layer was the highest(54.31t/hm2) in Prunus salicina,and TN storage in the topsoil layer was the highest(6.21t/hm2) in Passiflora caerulea.Both SOC and TN storage were the lowest in Punica granatum,with 49.77t/hm2 and 5.66t/hm2 respectively.Prunus salicina and Passiflora caerulea were both comparative better vegetation restoration patterns in the process of vegetation restoration and reconstruction in the rocky desertification region of Guizhou Province.

参考文献

[1] 刘丛强.生物地球化学过程与地表物质循环——西南喀斯特土壤-植被系统生源要素循环[M].科学出版社,2009.
[2] 吴秀芹,蔡运龙.我国亚热带喀斯特生态环境演变研究进展[J].自然科学进展,2006,16(3):267-272.
[3] 张俊华,常庆瑞,贾科利,等.黄土高原植被恢复对土壤肥力质量的影响研究[J].水土保持学报,2003,17(4):38-41.
[4] 黄和平,杨吉力,毕军,等.皇甫川流域植被恢复对改善土壤肥力的作用研究[J].水土保持学报,2005,25(3):37-40.
[5] 张杨,梁爱华,王平平,等.黄土丘陵区不同植被恢复模式下土壤养分效应[J].西北农业学报,2010,19(9):114-118.
[6] 王国梁,刘国彬,刘芳,等.黄土沟壑区植被发育过程中植物群落组成及结构变化[J].生态学报,2003,23(12):2551-2557.
[7] 程积民,万惠蛾,胡相明.黄土丘陵区植被恢复重建模式与演替过程研究[J].草地学报,2005,13(4):324-328.
[8] 龙健,黄昌勇,李娟.喀斯特山区土地利用方式对土壤质量演变的影响[J].水土保持学报,2002,6(1):76-79.
[9] 何宁,宋同清,彭晚霞,等.喀斯特峰丛洼地次生林土壤有机碳的剖面分布特征[J].植物营养与肥料学报,2012,18(2):374-381.
[10] 徐杰,邓湘雯,方晰,等.湘西南石漠化地区不同植被恢复模式的土壤有机碳研究[J].水土保持学报,2012,26(6):171-179.
[11] 李菲,李娟,龙健,等.典型喀斯特山区植被类型对土壤有机碳、氮的影响[J].生态学杂志,2015,34(12):3374-3381.
[12] Hu Shuijin,Coleman D C,Carroll C R,et al.Labile soil carbon pools in subtropical forest and agricultural ecosystems as influenced by management practices and vegetation patterns[J].Agriculture,Ecosystems and Enviroment,1997,65:69-78.
[13] Van Noordwijk M,Cerri C,Woomer P L,et al.Soil carbon dynamics in the humid tropical forest zone[J].Geodema,1997,79:187-225.
[14] Rutigliano F A,Ascoli R D.Soil microbial metabolism and nutrient status in a Mediterranean area as affectd by plant cover[J].Soil Biology and Biochemistry,2004,36:1719-1729.
[15] Fu Xiaoli,Shao Mingan,Wei Xiaorong,et al.Soil organic carbon and total nitrogen as effected by vegetation patterns in Northern Loess Plateau of China[J].Geoderna,2010,155:31-35.
[16] Kirkby E A.Plant growth in relation to nitrogen supply[J].Ecological Bulletins,1981,33:249-267.
[17] 从怀军,成毅,安韶山,等.黄土丘陵区不同植被恢复措施对土壤养分和微生物量C、N、P的影响[J].水土保持学报,2010,24(4):217-221.
[18] 董云中,王永亮,张建杰,等.晋西北黄土高原丘陵区不同土地利用方式下土壤碳氮储量[J].应用生态学报,2014,25(4):955-960.
[19] 贾晓红,李新荣,周玉燕,等.干旱沙区人工固沙植被演变过程中土壤有机碳氮储量及其分布特征[J].环境科学,2012,33(3):938-945.
[20] 贾晓红,李新荣,李元寿.干旱沙区植被恢复中土壤碳氮变化规律[J].植物生态学报,2007,31(1):1-4.
[21] 白军红,丁秋祎,高海峰,等.向海湿地不同植被群落下土壤氮素的分布特征[J].地理科学,2009,29(3):381-383.
[22] 漆良华,张旭东,周金星,等.湘西北小流域不同植被恢复区土壤微生物数量、生物量碳氮及其分形特征[J].林业科学,2009,45(8):14-20.
[23] 王志齐,杜兰兰,赵慢,等.黄土丘陵区不同退耕方式下土壤碳氮的差异及其影响因素[J].应用生态学报,2016,27(3):716-722.
[24] Jobbagy E G,Jackson R B.The vertical distribution of soil organic carbon and its relation to climate and vegetation[J].Ecological Applications,2000,10:423-436.
[25] 李海防,夏汉平,熊艳梅,等.土壤温室气体产生与排放影响因素研究进展[J].生态环境,2007,16(6):1781-1788.
[26] 翁伯琦,郑祥洲,丁洪,等.植被恢复对土壤碳氮循环的影响研究进展[J].应用生态学报,2013,24(12):3610-3616.
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