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天山北坡不同环境条件下雪岭云杉(Picea schrenkiana)林限土壤属性
引用本文:陈曦,许文强,罗格平,蔺卿,肖鲁湘.天山北坡不同环境条件下雪岭云杉(Picea schrenkiana)林限土壤属性[J].生态学报,2008,28(1):53-61.
作者姓名:陈曦  许文强  罗格平  蔺卿  肖鲁湘
作者单位:1. 中国科学院新疆生态与地理研究所,乌鲁木齐,830011
2. 中国新疆水利水电规划设计管理局,乌鲁木齐,830000
3. 中国科学院遥感应用研究所,北京,100101
基金项目:中国科学院西部之光联合学者资助项目 , 国家自然科学基金
摘    要:为了研究干旱区天山北坡中山带长达1000余公里的单建群种山地针叶林的空间分布原因,选择精河、玛纳斯、阜康和巴里坤中山带作为四种不同的环境条件,通过对不同环境条件雪岭云杉(Picea schrenkiana)上、下限土壤的采样与分析,探讨土壤因素对天山北坡中山带雪岭云杉分布的控制作用.雪岭云杉在天山北坡的连续分布主要是水热组合条件和土壤因素相互作用的结果,上、下限土壤属性变化与环境条件变化间存在着紧密的联系,表现为降雨量丰富的玛纳斯林区土壤肥力较高,但CaCO3含量较低,而降雨量较小的巴里坤和精河林区土壤肥力较差,但CaCO3含量较高.虽然长达1000余公里的雪岭云杉中山带环境条件差异较大,但其土壤属性变化均在雪岭云杉发育所需土壤条件的允许范围之内,这主要是受土壤成土母质、不同海拔高度的降雨量、地形、局地环流等因素的共同影响.

关 键 词:雪岭云杉  水热组合条件  土壤属性  林限  天山北坡  天山北坡  环境条件变化  雪岭云杉  土壤属性  Tianshan  mountains  slope  northern  conditions  environmental  response  forests  tree  properties  影响  因素  局地环流  不同海拔高度  土壤成土母质  允许范围  土壤条件
文章编号:1000-0933(2008)01-0053-09
收稿时间:2007-05-14
修稿时间:2007-10-30

Soil properties at the tree limits of Picea schrenkiana forests in response to varying environmental conditions on the northern slope of Tianshan mountains
CHEN Xi,XU Wenqiang,LUO Geping,LIN Qing and XIAO Luxiang.Soil properties at the tree limits of Picea schrenkiana forests in response to varying environmental conditions on the northern slope of Tianshan mountains[J].Acta Ecologica Sinica,2008,28(1):53-61.
Authors:CHEN Xi  XU Wenqiang  LUO Geping  LIN Qing and XIAO Luxiang
Institution:Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China;Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China;Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China;Xinjiang Water Resources Planning Administration,Urumqi 830000, China;Institute of Remote Sensing Applications,Chinese Academy of Sciences,Beijing 100101, China
Abstract:Coniferous forests consisting predominantly of Picea schrenkiana occur continuously,forming an unbroken,1000 km forest zone extending from west to east on the northern slope of Tianshan mountains where conditions such as precipitation,temperature and terrain vary greatly.To gain insights into the role of pedological process in controlling the growth of P.schrenkiana,soil under the forests was studied along 4 transects located at Jinghe,Manasi,Fukang and Balikun where the natural conditions are typical and,therefore,representative for western,central and eastern Tianshan mountains.On the transects,soil samples were taken in the area near the upper and lower tree limits of the forest zone.The continuous distribution of P.schrenkiana on the northern slope of Tianshan mountains is a result of combined water-heat conditions and pedological factors.At the upper and lower tree limits where difference exists in soil parent material,precipitation,topography,combined water-heat conditions and local atmospheric pattern,the soil properties show a close relationship with the local conditions.Because of the presence of high precipitation over the Manasi transect,the soil is fertile and low in CaCO3 content.In contrast,low soil fertility with high CaCO3 is seen in the soil on the Jinghe and Balikun transects where low precipitation exists.Although soil properties vary spatially due to the presence of different environmental conditions across the 1000 km forest zone on the northern slope of Tianshan mountains,soil is suitable for P.schrenkiana to grow.This study indicates that soil plays an important role in controlling the continuous distribution of the P.schrenkiana forests on the northern slope of Tianshan mountains.
Keywords:Picea schrenkiana  combined water-heat conditions  soil properties  upper and lower tree limits  northern slope of Tianshan mountains
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