首页 | 本学科首页   官方微博 | 高级检索  
     

黄土丘陵区退耕地生物结皮理化性状初报
引用本文:赵允格,许明祥,王全九,邵明安. 黄土丘陵区退耕地生物结皮理化性状初报[J]. 应用生态学报, 2006, 17(8): 1429-1434
作者姓名:赵允格  许明祥  王全九  邵明安
作者单位:1. 中国科学院水利部水土保持研究所黄土高原土壤侵蚀与旱地农业国家重点实验室,杨凌,712100;西北农林科技大学,杨凌,712100
2. 中国科学院水利部水土保持研究所黄土高原土壤侵蚀与旱地农业国家重点实验室,杨凌,712100;中国科学院地理科学与资源研究所,北京,100101
基金项目:中国科学院"西部之光"人才培养计划;国家自然科学基金;中国科学院基金
摘    要:通过野外调查并结合室内分析,研究了黄土丘陵区阴坡不同年限退耕地土壤生物结皮的盖度、厚度、容重、粘结力以及结皮土壤的有机质、养分含量等理化性质.结果表明,研究区耕地退耕后首先出现由降雨打击而形成的结构结皮,其后随退耕年限的延长,结皮生物逐渐迁入,与土壤复合逐步演化为生物结皮.生物接皮面积随着高等植被盖度的增加有降低的趋势;厚度随退耕年限的延长呈倒S型增加,退耕10年后,结皮厚度增加缓慢;容重随退耕年限的延长而减小.结皮的形成可显著增强土壤粘结力,结皮层粘结力随退耕年限的延长呈倒S型增长.结皮土壤有机质、全氮含量明显高于研究区耕地土壤,且随退耕年限的延长而增加;退耕10年后,结皮土壤有机质及全氮含量趋于稳定.结皮土壤全磷含量与农地耕层土壤相当.生物结皮的形成提高了土壤速效氮、磷、钾含量.研究区阴坡退耕地土壤结皮的形成大致可分为3个阶段:退耕1~4年为结皮初始形成期,5~10年为结皮快速发育期,10年以后为稳定期.

关 键 词:黄土丘陵区  退耕地  生物结皮  理化性状
文章编号:1001-9332(2006)08-1429-06
收稿时间:2005-08-11
修稿时间:2006-06-16

Physical and chemical properties of soil bio-crust on rehabilitated grassland in hilly Loess Plateau of China
ZHAO Yunge,XU Mingxiang,WANG Quanjiu,SHAO Ming'an. Physical and chemical properties of soil bio-crust on rehabilitated grassland in hilly Loess Plateau of China[J]. The journal of applied ecology, 2006, 17(8): 1429-1434
Authors:ZHAO Yunge  XU Mingxiang  WANG Quanjiu  SHAO Ming'an
Affiliation:1 State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences, Yangling 712100, China; 2Northwest Sci-Tech University of Agriculture and Forestry, Yangling 712100, China; 3Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
Abstract:Soil bio-crust (SBC) plays an important role in degraded ecosystem restoration. The field investigation and laboratory analysis of SBC on different year rehabilitated grasslands at the north slope of hilly Loess Plateau showed that after cropland shifted to rehabilitated grassland, rainfall- induced structural crust appeared firstly, and then, with the increasing year of rehabilitation, crust- forming microorganism gradually settled in, and SBC developed. The depth of SBC increased in inverse "S" shape with increasing year of rehabilitation. 10 years after rehabilitation, the increase of SBC depth slowed down, and soil bulk density decreased from 1.4 g x cm(-3) to 1.1 g x cm(-3). SBC formation improved soil cohesion significantly, and the latter was increased in inverse "S" shape with increasing year of rehabilitation. The organic matter and total nitrogen contents in SBC were obviously higher than those in cropland, and increased gradually with increasing year of rehabilitation but tended to be stable after 10 years of rehabilitation. The available N, P and K contents in SBC were also increased, but no significant difference of total phosphorus was found between SBC and cropland soil. The formation of SBC in test region could be classified into 3 stages, i. e., the first stage named the beginning of the formation, which was from 1 to 4 years of grassland rehabilitation, the second stage named the rapid development period, which was from 5 to 10 years of the rehabilitation, and the third stage named stable period after 10 years of rehabilitation.
Keywords:Hilly Loess Plateau   Rehabilitated grassland   Soil bio-erust   Physical and chemical properties.
本文献已被 CNKI 维普 万方数据 等数据库收录!
点击此处可从《应用生态学报》浏览原始摘要信息
点击此处可从《应用生态学报》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号