Please use this identifier to cite or link to this item: http://hdl.handle.net/11455/74029
DC FieldValueLanguage
dc.contributor.author李振州zh_TW
dc.contributor.author譚鎮中zh_TW
dc.contributor.author吳道仁zh_TW
dc.contributor.other國立中興大學農學院實驗林管理處zh_TW
dc.date2003-09zh_TW
dc.date.accessioned2014-06-12T09:28:05Z-
dc.date.available2014-06-12T09:28:05Z-
dc.identifier.urihttp://hdl.handle.net/11455/74029-
dc.description.abstract土壤有機質是生態系初級生產量的主要組成,本文闡述臺灣中部關刀溪森林生態系之土壤有機質與土壤呼吸量之境況,以瞭解土壤有機質在生態系之碳循環中的角色與變化。在穿越集水區不同林分的人行步道上劃設的採樣點,分別取樣並帶回分析其中有機碳與氮等營養含量,以及現場量測土壤表面二氧化碳的釋放速率。落葉層中總碳含量從220到550 g C m??,而土壤層則為18.2到41.4 kg C m??;總氮含量則分別為4.5?13.9 g N m??與1.62?3.74 kg N m??,進一步計算其碳氮比,落葉層為32?79,zh_TW
dc.description.abstractThe soil organic matter is a major constituent of the primary production of ecosystem. The soil nutrient contents and soil respiration were monitored at Guandaushi Forest Ecosystem Research Station, Taiwan to understand the fate and role of soil organicen_US
dc.language.isoen_USzh_TW
dc.publisher臺中市: 國立中興大學農學院實驗林管理處zh_TW
dc.relation林業研究季刊, Volume 25, Issue 3, Page(s) 1-10.zh_TW
dc.subject土壤有機質zh_TW
dc.subject二氧化碳通量zh_TW
dc.subject森林生態系zh_TW
dc.titleThe+Turnover+of+Soil+Organic+Matter+and+the+Flux+of+Soil+Carbon+Dioxide+at+Guandaushi+Forest+Ecosystemen_US
dc.title關刀溪森林生態系土壤有機質週轉率與土壤呼吸通量zh_TW
dc.typeJournal Articlezh_TW
item.openairetypeJournal Article-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.languageiso639-1en_US-
item.grantfulltextrestricted-
item.fulltextwith fulltext-
item.cerifentitytypePublications-
Appears in Collections:第25卷 第03期
農業暨自然資源學院
Files in This Item:
File SizeFormat Existing users please Login
143810-1.pdf460.61 kBAdobe PDFThis file is only available in the university internal network   
Show simple item record
 

Google ScholarTM

Check


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.