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黄土丘陵区小流域土地利用对土壤有机碳和全氮的影响
引用本文:王小利,郭胜利,马玉红,黄道友,吴金水.黄土丘陵区小流域土地利用对土壤有机碳和全氮的影响[J].应用生态学报,2007,18(6):1281-1285.
作者姓名:王小利  郭胜利  马玉红  黄道友  吴金水
作者单位:1. 贵州大学生命科学学院,贵阳,550025;西北农林科技大学资源环境学院,陕西杨凌,712100
2. 西北农林科技大学资源环境学院,陕西杨凌,712100;中国科学院水利部水土保持研究所,陕西杨凌,712100
3. 中国科学院水利部水土保持研究所,陕西杨凌,712100
4. 中国科学院亚热带农业生态研究所,长沙,410125
基金项目:中国科学院"西部之光"人才培养计划;中国科学院知识创新工程项目
摘    要:通过野外调查和室内分析,研究了黄土丘陵沟壑区燕沟流域农地、果园、林地和草地0~20cm表层土壤的有机碳(SOC)和全氮(TSN)积累特征.结果表明:该区SOC含量平均值为7·56g·kg-1,TSN平均值为0·71g·kg-1.其中,农地SOC和TSN平均值分别为4·67和0·48g·kg-1,且梯田较低,川坝地较高.与农地相比,果园SOC(4·33g·kg-1)和TSN(0·46g·kg-1)平均值略有降低,草地较高.林地SOC和TSN平均值较农地高117·7%和89·4%.该区SOC和TSN含量的变异系数为69·7%和58·4%,以林地最大(62·8%和54·5%),草地和农地次之,果园最小(18·0%和22·9%).土壤C/N依果园、农地、草地和林地的顺序递增.该区各类土地利用方式下的SOC和TSN都呈极显著正相关(r=0·9791).黄土丘陵沟壑区基本农田建设和果园建设对SOC和TSN积累作用不明显;退耕还林还草、封山育林等土地利用优化措施明显促进了SOC和TSN的积累.

关 键 词:潜力-约束模型  建设用地适宜性  情景分析  敏感性分析  冀中南  
文章编号:1001-9332(2007)06-1281-05
修稿时间:2006-04-032007-03-20

Effects of land use type on soil organic C and total N in a small watershed in loess hilly-gully region
WANG Xiao-li,GUO Sheng-li,MA Yu-hong,HUANG Dao-you,WU Jin-shui.Effects of land use type on soil organic C and total N in a small watershed in loess hilly-gully region[J].Chinese Journal of Applied Ecology,2007,18(6):1281-1285.
Authors:WANG Xiao-li  GUO Sheng-li  MA Yu-hong  HUANG Dao-you  WU Jin-shui
Institution:College of Life Science, Guizhou University, Guiyang 550025, China. djjwxl@yahoo.com.cn
Abstract:Based on field survey and laboratory analysis, this paper studied the storage of surface soil (0-20 cm) organic C (SOC) and total N (TSN) in farmland, orchard, woodland and grassland in the Yangou watershed of loess hilly-gully region. The results showed that in the test area, the mean contents of SOC and TSN were 7.56 and 0.71 g . kg(-1), respectively. On an average, farmland had 4.67 g . kg(-1) of SOC and 0.48 g . kg(-1) of TSN, and terrace farmland had lower storage of SOC and TSN than other types of farmland. Compared with farmland, the contents of SOC and TSN in orchard had a slight decrease, being 4. 33 g . kg(-1) and 0.46 g . kg(-1), respectively, while those in grassland were higher. The average contents of SOC and TSN in woodland were 117.7% and 89.4% higher than those in farmland. In this area, the variation coefficients of SOC and TSN contents were 69.7% and 58.4%, respectively, being the highest (62.8% and 54.5%) in woodland, the second in grassland and farmland, and the smallest (18.0% and 22.9%) in orchard. Soil C/N ratio was increased in the order of orchard, farmland, grassland, woodl and. Under these four landuse types, there was a significant positive correlation between SOC and TSN (r = 0.9791). The construction of farmland and orchard didn' t increase the contents of SOC and TSN significantly, while the conversion of farmland into woodland or grassland and the hill-closure forestry promoted the accumulation of SOC and TSN distinctly.
Keywords:land use  soil organic C  total N  loess hilly-gully region  
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