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Proceedings of International Conference on Climate Change, Biodiversity and Ecosystem Services for the Sustainable Development Goals : Policy and Practice 27-29 June 2016 at the Sirindhorn International Environmental Park, Cha-am, Phetchaburi, Thailand

I.  INTRODUCTION  Ecosystem  services  are  part  of  the  2030  Agenda  for  Sustainable  Development  and  Sustainable  Development  Goals  (SDGs)  especially  SDG  15  (managing  sustainable  forest,  combating  desertification,  halting  land  degradation  and  biodiversity  loss)  1.  An  important  ecosystem  service  is  absorbing  CO2  from  atmosphere  into  forests  by  photosynthesis  process  as  a  CO2  sink.  However,  forests  also  release  CO2  to  atmosphere  by  plant  and  soil  respiration  processes  as  a  CO2  source. Soil  respiration  (Rs)  or  soil  CO2  emission  which  produces  CO2  by  soil  organisms  and  underground  parts  of  plants  in  forests  is  an  important  component  of  ecosystem  respiration  (Re).  Moreover,  the  amount  of  this  CO2  exchange  is  important  in  our  understanding  response  of  forest  during  climate  variability  such  as  the  effects  of  heavy  rainfall  events  and  extended  dry  periods.  Dynamically,  soil  CO2  emissions  occur  during  both  non-steady  state  (with  disturbances)  and  steady  state  (without  disturbances)  2,  and  understanding  the  emissions  during  both  states  is  crucial  to  help  us  quantify  soil  respiration.  The  fast  response  of  CO2  emission  to  these  environmental  changes  and  disturbances  could  be  causes  of  uncertainty  associated  with  CO2  emission  quantification  3-9.  Therefore,  enhancing  accuracy  in  assessment  of  soil  CO2  emission  in  forest  is  desired  in  order  to  improve  our  understanding  of  forest  carbon  exchange,  its  source-sink  capacity  and  its  responses  to  climate  change/variability.  Although,  most  of  researchers  in  the  past  had  used  chamber  method  (conventional  method)  because  it  is  economical  and  easy-to-use,  some  conventional  methods  could  not  detect  phenomena  of  soil  respiration  responses  during  such  disturbances.  On  the  other  hand,  soil  gradient  method  using  CO2  sensor  as  a  newly  established  technique  could  improve  the  accuracy  of  the  CO2  quantification  together  with  capturing  its  responses  to  disturbance  including  variability  in  climate  8-9.The  sensor  method  was  found  to  yield  a  very  close  result  to  that  obtained  by  chamber  measurements  4-5,  8.  A  good  correlation  between  the  two  techniques  was  also  reported  6.  Therefore,  this  study  aims  to  measure  soil  CO2  by  the  newly  established  method  using  CO2  profile  gradient  (continuously  and  frequently  recorded  every  15  seconds  and  averaged  every  15  minutes)  and  to  study  variations  in  soil  CO2  effluxes  in  a  dry  dipterocarp  forest  and  a  mixed  deciduous  forest.  The  monitoring  using  the  soil  CO2  probes  also  enabled  us  to  clearly  see  the  behaviors  of  soil  CO2  emission  during  climate  variability. II. MATERIALS  AND  METHODS A.  Site  Description The  study  sites  were  located  in  a  dry  dipterocarp  forest  and  a  mixed  deciduous  forest.  These  are  among  the  two  of  the  AsiaFlux  network’s  sites  in  Thailand.  Both  sites  are  tropical  monsoon  forest.  The  first  study  site  was  known  as  DFR  site  (a  Dry  Dipterocarp  Forest  Flux  Ratchaburi),  King  Mongkut’s  University  of  Technology  Thonburi  (KMUTT),  Ratchaburi  Campus,  Rang  Bour,  Chombueng,  Ratchaburi,  western  Thailand  (Latitude:  13º  35’  13.3”  N,  Longitude:  99º  30’  3.9”  E).Another  site  was  MKL  site  (Mae  Klong Watershed  Research  Station),  Thong  PhaPhoom,  Kanchanaburi,  western  Thailand  (Latitude:  14º  34’  34.6”  N,  Longitude:  98º  50’  38.0”  E).  The  DFR  site  had  been  kept  as  the  dry  dipterocarp  forest  for  approximately  50  years  but  communities  have  exploited  for  timber  and  charcoal  raw  material  harvests.  As  a  result,  most  of  trees  in  this  forest  were  regenerated  and  ages  of  the  trees  were  6-7  years  (measurement  in  2011).  The  DFR  site  was  situated  at  118  m  elevation.  The  vegetation  type  was  a  dry  dipterocarp  forest  and  the  dominant  species  were  Dipterocarpus  intricate,  152 Proceedings  of  the  International  Conference  on  Climate  Change,  Biodiversity  and  Ecosystem  Services  for  the Sustainable  Development  Goals  (SDGs):  Policy  and  Practice  27-29  June  2016,  Cha-am,  Phetchaburi,  Thailand


Proceedings of International Conference on Climate Change, Biodiversity and Ecosystem Services for the Sustainable Development Goals : Policy and Practice 27-29 June 2016 at the Sirindhorn International Environmental Park, Cha-am, Phetchaburi, Thailand
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