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粤北石漠化地区水文过程试验研究
  • ISSN号:1000-0690
  • 期刊名称:地理科学
  • 时间:2013.4.15
  • 页码:481-488
  • 分类:S153.62[农业科学—土壤学;农业科学—农业基础科学]
  • 作者机构:[1]佛山科学技术学院,广东佛山528000, [2]中山市第二中学,广东中山528429, [3]佛山顺德一中德胜学校,广东顺德528333, [4]佛山张槎中学,广东佛山,528000, [5]华南师范大学地理科学学院,广东广州510631
  • 相关基金:国家自然科学基金(31170486)、广东省自然科学基金(S2012010009272)和中国科学院西部行动项目“西南喀斯特生态系统服务功能维持机理与调控技术研究”(KZCX2-XB3-10)
  • 相关项目:粤北岩溶山区岩石-土壤-植物系统钙迁移循环过程及其生态效应
中文摘要:

为掌握石漠化对岩溶地表土壤碳量的影响,选择粤北英德市岩背镇塘边村岩溶峰丛不同石漠化程度样地进行系统调查,采用单位面积土壤有机碳指标分析石漠化过程对土壤有机碳储量影响。结果表明:(1)极重度石漠化使土壤厚度、地表生物量显著减少,使岩石裸露率显著增加,但在潜在、轻度至中度石漠化中,差异不显著;(2)极重度石漠化土壤有机碳含量显著高于其他石漠化,中度石漠化土壤有机碳高于轻度石漠化,轻度高于潜在,但差异不显著;(3)10-20 cm 土层有机碳含量明显低于表层,岩石裸露及土壤主要在溶蚀缝隙中分布和发育是造成极重度和中度石漠化单位重量土壤有机碳增加的主要原因;(4)中度、轻度和潜在石漠化单位面积土壤有机碳分别是极重度的49.23倍、47.9倍和29.4倍;(5)岩石裸露率是影响岩溶地表生态的最主要因素,它和地表生物量之间存在极显著的负相关,与单位面积土壤有机碳总量呈显著的负相关关系,和土壤厚度也存在显著的负相关关系,此外,岩溶植物的高度适应性可以削弱石漠化的影响。

英文摘要:

In order to analyze the effect of rocky desertification on the storage of soil organic carbon,sample plots with different degrees of rock desertification in a typical karst peak-cluster in the Tangbian village, Yanbei town,Yingde City,the north of Guangdong Province are selected in this paper,and a new index of unit area soil organic carbon is adopted in the analysis on the effect of rocky desertification process to the or-ganic carbon storage.The results show that:(1)The thickness of soil and standing biomass decreased sig-nificantly and the rock coverage increased significantly in intense rock desertification,but the difference are not significant between potential,slight and medium rock desertification in soil thickness,standing biomass and rock coverage.(2)Obviously,organic carbon content per unit of soil weigh is highest in intense rock de-sertification plots.It is higher in medium than in slight rock desertification plots,and it is higher in slight than in potential desertification plots,but the difference is not significant between medium,slight and poten-tial rock desertification.(3)The soil organic carbon content in 10 -20 cm soil depth is lower than that in 0-10 cm.Water and soil losing leads rocky coverage increase and only a little soil remain in the fissure of rock,those micro-negative relief can capture organic matter,that may be the major cause for the increase of soil organic carbon in intense and medium rock desertification.(4)The soil organic carbon content per unit area of in medium,slight and potential rock desertification is 49.23,47.9 and 29.4 times of that in intense rock desertification.(5 )The rock coverage is the main factor that impacting the karst ecological system. There is significant negative correlation between the rock coverage and the ground biomass,between the rock coverage and unit area of soil organic carbon,and between the rock coverage and thickness of soil.Highly a-daptive plants in karst area can weaken the effects on soil organic carbon by rock deser

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期刊信息
  • 《地理科学》
  • 北大核心期刊(2011版)
  • 主管单位:中科院
  • 主办单位:中国科学院 东北地理与农业生态研究所
  • 主编:陆大道
  • 地址:长春市高新北区盛北大街4888号
  • 邮编:130012
  • 邮箱:geoscien@iga.ac.cn
  • 电话:0431-85542212 85542217
  • 国际标准刊号:ISSN:1000-0690
  • 国内统一刊号:ISSN:22-1124/P
  • 邮发代号:8-31
  • 获奖情况:
  • 中国自然科学核心期刊,中国地理学会优秀地理期刊
  • 国内外数据库收录:
  • 俄罗斯文摘杂志,荷兰文摘与引文数据库,美国剑桥科学文摘,日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版),中国北大核心期刊(2000版)
  • 被引量:39183