茶叶科学
茶葉科學
다협과학
2015年
3期
263-270
,共8页
王峰%陈玉真%尤志明%吴志丹%江福英%翁伯琦%张文锦
王峰%陳玉真%尤誌明%吳誌丹%江福英%翁伯琦%張文錦
왕봉%진옥진%우지명%오지단%강복영%옹백기%장문금
茶园%土壤类型%土壤腐殖质%剖面分布
茶園%土壤類型%土壤腐殖質%剖麵分佈
다완%토양류형%토양부식질%부면분포
tea garden%soil types%soil humus%profile distribution
采用野外调查和室内分析相结合的方法,对武夷山市5种主要土壤类型(黄壤、红壤、潮砂土、高山草甸土、紫色土)茶园的土壤腐殖质剖面分布特征进行研究。结果表明,茶园土壤腐殖质各组分含量基本随着土层加深呈减少趋势。不同类型茶园土壤腐殖质的含量和组成存在显著差异,高山草甸土茶园土壤腐殖质及各组分的含量均显著高于其他土壤类型,黄壤和紫色土次之,红壤最低。土壤腐殖质组成中,均以胡敏酸比例最高(57.06%~79.76%),除高山草甸土外,各土壤中富里酸比例均大于胡敏酸。茶园土壤富里酸的色调系数(△logK)和光密度值(E4/E6)均大于胡敏酸,高山草甸土富里酸和胡敏酸的△logK 和 E4/E6值最低,土壤腐殖化复杂程度最高;红壤的富里酸和胡敏酸的△logK 和 E4/E6值最高,土壤腐殖质复杂程度及化学稳定性低。相关分析表明,土壤腐殖质组成与土壤有机碳、酚类含量、全氮、土壤容重和孔隙度存在显著相关性,与土壤 C/N、pH 和含水率相关性不明显。可见,茶园土壤腐殖质均以胡敏素为主,高山草甸土为胡敏酸型,其余土壤为富里酸型。
採用野外調查和室內分析相結閤的方法,對武夷山市5種主要土壤類型(黃壤、紅壤、潮砂土、高山草甸土、紫色土)茶園的土壤腐殖質剖麵分佈特徵進行研究。結果錶明,茶園土壤腐殖質各組分含量基本隨著土層加深呈減少趨勢。不同類型茶園土壤腐殖質的含量和組成存在顯著差異,高山草甸土茶園土壤腐殖質及各組分的含量均顯著高于其他土壤類型,黃壤和紫色土次之,紅壤最低。土壤腐殖質組成中,均以鬍敏痠比例最高(57.06%~79.76%),除高山草甸土外,各土壤中富裏痠比例均大于鬍敏痠。茶園土壤富裏痠的色調繫數(△logK)和光密度值(E4/E6)均大于鬍敏痠,高山草甸土富裏痠和鬍敏痠的△logK 和 E4/E6值最低,土壤腐殖化複雜程度最高;紅壤的富裏痠和鬍敏痠的△logK 和 E4/E6值最高,土壤腐殖質複雜程度及化學穩定性低。相關分析錶明,土壤腐殖質組成與土壤有機碳、酚類含量、全氮、土壤容重和孔隙度存在顯著相關性,與土壤 C/N、pH 和含水率相關性不明顯。可見,茶園土壤腐殖質均以鬍敏素為主,高山草甸土為鬍敏痠型,其餘土壤為富裏痠型。
채용야외조사화실내분석상결합적방법,대무이산시5충주요토양류형(황양、홍양、조사토、고산초전토、자색토)다완적토양부식질부면분포특정진행연구。결과표명,다완토양부식질각조분함량기본수착토층가심정감소추세。불동류형다완토양부식질적함량화조성존재현저차이,고산초전토다완토양부식질급각조분적함량균현저고우기타토양류형,황양화자색토차지,홍양최저。토양부식질조성중,균이호민산비례최고(57.06%~79.76%),제고산초전토외,각토양중부리산비례균대우호민산。다완토양부리산적색조계수(△logK)화광밀도치(E4/E6)균대우호민산,고산초전토부리산화호민산적△logK 화 E4/E6치최저,토양부식화복잡정도최고;홍양적부리산화호민산적△logK 화 E4/E6치최고,토양부식질복잡정도급화학은정성저。상관분석표명,토양부식질조성여토양유궤탄、분류함량、전담、토양용중화공극도존재현저상관성,여토양 C/N、pH 화함수솔상관성불명현。가견,다완토양부식질균이호민소위주,고산초전토위호민산형,기여토양위부리산형。
Based on the field survey and laboratory analysis, the soil humus composition in five soil types (yellow soil, red earth, moisture sandy soil, alpine meadow soil and purple soil) of tea garden in Wuyishan city were investigated. The results showed that the content of humic acid(HA), fulvic acid(FA) and Humin(HM) decreased with the soil depth. There were significant differences of humus composition among different soil types. The humus composition and carbon level in alpine meadow soil of tea garden were significantly higher than those in other soil types, followed by those in yellow soil and purple soil, the lowest was in red soil. Humin was the main composition of humus(57.06%-79.76%). Except alpine meadow soil, the proportion FA were more than those in HA. The△log K and E4/E6 value of FA was higher than HA. The△log K and E4/E6 value in alpine meadow soil and red soil were the lowest and highest, respectively. The soil humus composition were significantly correlated with soil organic carbon and phenol contents, total N, soil bulk density and soil porosity, but no significant correlated with C/N, pH value and soil moister. Thus, the major type of humus was humin in all five kinds of tea garden soils, alpine meadow soil belonged to the humic acid type soil, and others belonged to fulvic acid enriched soil.