东北林业大学学报
東北林業大學學報
동북임업대학학보
JOURNAL OF NORTHEAST FORESTRY UNIVERSITY
2009年
11期
92-95
,共4页
孙晓新%牟长城%闵长林%刘霞%吴云霞%冯登军%石兰英%程伟
孫曉新%牟長城%閔長林%劉霞%吳雲霞%馮登軍%石蘭英%程偉
손효신%모장성%민장림%류하%오운하%풍등군%석란영%정위
小兴安岭%湿地%CH_4通量%日变化%温度%水位
小興安嶺%濕地%CH_4通量%日變化%溫度%水位
소흥안령%습지%CH_4통량%일변화%온도%수위
Xiaoxing'an mountains%Diurnal variations%Methane fluxes%Temperatures%Water table%Wetlands
利用静态暗箱-气相色谱法,研究了小兴安岭7种沼泽类型生长季初期、中期、末期甲烷(CH_4)通量的日变化规律,结果表明:小兴安岭沼泽甲烷通量无统一的日变化规律,且与温度和水位两个环境因子的相关性较弱.7个沼泽类型中,仅毛赤杨(Alnus sibirica)沼泽和白桦(Betula platyphylla)沼泽甲烷通量峰值在生长季初期、中期、末期出现的时间大致相同,且都为单峰曲线;苔草(Carex schmidtii)沼泽、灌丛沼泽和落叶松(Larix gmelinii)-泥炭藓(Sphagnum spp.)沼泽甲烷通量的峰值在不同时期出现的时间不同,多数为单峰曲线;落叶松-苔草沼泽和落叶松-藓类沼泽甲烷通量速率较小,多数时间吸收甲烷,没有明显的日变化规律.不同类型沼泽和生长期之间甲烷通量没有统一的日变化规律,说明在进行区域甲烷排放总量的估测时,增加每天的观测频率,或者长期、大量的观测数据可能会对提高估测精度有很大帮助.
利用靜態暗箱-氣相色譜法,研究瞭小興安嶺7種沼澤類型生長季初期、中期、末期甲烷(CH_4)通量的日變化規律,結果錶明:小興安嶺沼澤甲烷通量無統一的日變化規律,且與溫度和水位兩箇環境因子的相關性較弱.7箇沼澤類型中,僅毛赤楊(Alnus sibirica)沼澤和白樺(Betula platyphylla)沼澤甲烷通量峰值在生長季初期、中期、末期齣現的時間大緻相同,且都為單峰麯線;苔草(Carex schmidtii)沼澤、灌叢沼澤和落葉鬆(Larix gmelinii)-泥炭蘚(Sphagnum spp.)沼澤甲烷通量的峰值在不同時期齣現的時間不同,多數為單峰麯線;落葉鬆-苔草沼澤和落葉鬆-蘚類沼澤甲烷通量速率較小,多數時間吸收甲烷,沒有明顯的日變化規律.不同類型沼澤和生長期之間甲烷通量沒有統一的日變化規律,說明在進行區域甲烷排放總量的估測時,增加每天的觀測頻率,或者長期、大量的觀測數據可能會對提高估測精度有很大幫助.
이용정태암상-기상색보법,연구료소흥안령7충소택류형생장계초기、중기、말기갑완(CH_4)통량적일변화규률,결과표명:소흥안령소택갑완통량무통일적일변화규률,차여온도화수위량개배경인자적상관성교약.7개소택류형중,부모적양(Alnus sibirica)소택화백화(Betula platyphylla)소택갑완통량봉치재생장계초기、중기、말기출현적시간대치상동,차도위단봉곡선;태초(Carex schmidtii)소택、관총소택화락협송(Larix gmelinii)-니탄선(Sphagnum spp.)소택갑완통량적봉치재불동시기출현적시간불동,다수위단봉곡선;락협송-태초소택화락협송-선류소택갑완통량속솔교소,다수시간흡수갑완,몰유명현적일변화규률.불동류형소택화생장기지간갑완통량몰유통일적일변화규률,설명재진행구역갑완배방총량적고측시,증가매천적관측빈솔,혹자장기、대량적관측수거가능회대제고고측정도유흔대방조.
An experiment was conducted to observe the diurnal methane fluxes from seven types of wetlands in Xiaoxing' an Mountains using the static opaque chamber and gas chromatography techniques. Results showed that no common diurnal variations were found in all the wetlands, and the diurnal patterns were weakly correlated to temperature and water table. The same pattern of diurnal fluxes with unique peak for Alnus sibirica swamp and Betula platyphylla swamp was found, and the peak occurred at the same time of day in different seasons. Marsh, thicket swamp and Larix gnwlinii-Sphagnum spp. swamp mostly displayed a pattern of diurnal fluxes with unique peak, and the peak occurred at different time of day in dif-ferent seasons. No apparent diurnal variations were observed in Larix gmelinii-Carex schmidtii swamp and Larix gmelinii-moss swamp because of the low flux rates. No common diurnal variations in different seasons for all the wetlands indicated that more measurement frequency or long term and larger observational data should be helpful to the estimation of regional methane fluxes.