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[1]ZHANG Yang,LIU Hua,WANG De-xiang,et al.Study on Soil Physicochemical Properties along Forest Age of Pinus tabulaeformis Plantations[J].Research of Soil and Water Conservation,2012,19(03):82-85,89.

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Study on Soil Physicochemical Properties along Forest Age of Pinus tabulaeformis Plantations

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 19 Number of periods: 2012 03 Page number: 82-85,89 Column: Public date: 2012-06-20

Title:: Study on Soil Physicochemical Properties along Forest Age of Pinus tabulaeformis Plantations

Author(s):: ZHANG Yang¹, LIU Hua², WANG De-xiang¹, WANG Yu-chao¹, WU Hao¹, ZHANG Li-nan¹, HUANG Qing-ping¹; 1. College of Forestry, Northwest A & F University, Yangling, Shaanxi 712100, China;
2. Management Committee of Jinsi Grand Canyon, Shangnan, Shaanxi 726300, China

Keywords:: Pinus tabulaeformis; forest age; soil physicochemical properties

CLC:: S714.5

DOI:: -

Abstract:: In order to explore the impact of forest ages on the physicochemical characteristics of soil under pinus tabulaeformis plantation and compare the variation characteristics of the soil physicochemical characteristics under pinus tabulaeformis plantation of different forest age, typical sample zones were set in Shangluo in this study. The combination method of field investigation and laboratory analysis was adopted. The results showed that organic matter, total nitrogen and pH value reduced with the increase of the forest age among the soil depth of 0-20 cm and 20-40 cm. The other physical and chemical parameters also changed, but did not show obvious increase or decrease. Total nitrogen and pH value reduced with the increase of the forest age among the soil depth of 40-60 cm. Correlation analysis showed that there was a positive correlation between organic matter, total nitrogen and pH value, while an extremely significant correlation between total nitrogen and pH value was observed. There was no significantly correlation between the other physical and chemical propterties.

References:: [1] 李国雷,刘勇,李瑞生,等.油松人工林土壤质量的演变[J].林业科学,2008,44(9):76-81.
[2] 陈立新,陈祥伟,段文标.落叶松人工林凋落物与土壤肥力变化的研究[J].应用生态学报,1998,9(6):581-586.
[3] 吴钦孝,赵鸿雁,汪有科,黄土高原油松林地产流产砂及其过程研究[J].生态学报,1998,18(2):151-157.
[4] 景丽,朱志红,王孝安,等.秦岭油松人工林与次生林群落特征比较[J].浙江林学院学报,2008,25(6):711-717.
[5] 董学军,陈仲新,陈锦正.毛乌素沙地油松的水分关系参数随不同土壤基质的变化[J].植物生态学报,1999,23(5):385-392.
[6] 李国强,杨劼,内蒙古皇甫川流域油松蒸腾特点分析[J].内蒙古大学学报:自然科学版,2001,32(3):301-305.
[7] 翟洪波,李吉月,聂力水.油松的水力结构特征[J].林业科学,2003,39(2):14-20.
[8] 高甲荣,肖斌,桥山林区油松人工林营养元素分配与积累的研究[J].应用生态学报,2001,12(5):667-671.
[9] 王克勤,王斌瑞.集水造林防止人工植被土壤干化的初步研究[J].林业科学,1998,34(4):14-21.
[10] 赵鸿雁,吴钦孝,刘国彬.黄土高原人工油松林枯枝落叶层的水土保持功能研究[J].林业科学,2003,39(1):168-172.
[11] 郑景明,罗菊春,曾德慧.森林生态系统管理的研究进展[J].北京林业大学学报,2002,24(3):103-109.
[12] Asdak C,Jarvis P G,Gardingen P V.Evaporation of intercepted precipitation based on an energy balance in unlogged and logged forest areas of central Kalamanta,Indonesia[J].Agricultural and Forest Meteorology,1998,92(3):173-180.
[13] Beschta R L.Forest hydrology in the Pacific Northwest:additional research needs[J].Journal of the American Water Resources Association,1998,34(4):729-741.
[14] 刘世海,余新晓,于志民.密云水库集水区人工油松林水源保护林降水化学性质研究[J].应用生态学报,2001,12(5):697-700.
[15] 潘成忠,上官周平.黄土区次降雨条件下林地径流和侵蚀产沙形成机制:以人工油松林和次生山杨林为例[J].应用生态学报,2005,16(9):1597-1602.
[16] 向琼.商洛地区几种中草药田昆虫群落结构动态研究[D].陕西杨凌:西北农林科技大学,2005.
[17] 刘光崧.土壤理化分析与剖面描述[M].北京:中国标准出版社,1996.
[18] 胡小飞,陈伏生,葛刚,等.森林采伐对林地表层土壤主要特征及其生态过程的影响[J].土壤通报,2007,38(6):1213-1218.
[19] 谷会岩,金靖博,陈祥伟,等.采伐干扰对大兴安岭北坡兴安落叶松林土壤化学性质的影响[J].土壤通报,2009,40(2):272-275.
[20] 温远光.大河山中山植被恢复过程植物物种多样性的变化[J].植物生态学报,1998,22(1):33-40.
[21] 展军礼,窦春蕊,油松人工林对土壤特性影响的初步研究[J].植树造林,2007(9):48-49.
[22] 耿增超,张社奇,王国栋,等.黄土高原油松人工林地突然养分及化学性质的时空效应[J].西北农林科技大学学报:自然科学版,2006,34(8):98-104.
[23] 刘世全,高丽丽,蒲玉琳,等.西藏土壤磷素和钾素养分状况及影响因素[J].水土保持学报,2005,19(1):75-78.
[24] 张振国,黄建成,焦菊英,等.黄土丘陵沟壑区退耕地人工柠条林土壤养分特征及其空间变异[J].水土保持通报,2007,27(5):114-120.

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