山地学报
山地學報
산지학보
JOURNAL OF MOUNTAIN SCIENCE
2001年
1期
9-13
,共5页
张萍%刘宏茂%陈爱国%刘志秋%付永能
張萍%劉宏茂%陳愛國%劉誌鞦%付永能
장평%류굉무%진애국%류지추%부영능
轮歇系统%种植系统%退化%土壤微生物%土壤养分
輪歇繫統%種植繫統%退化%土壤微生物%土壤養分
륜헐계통%충식계통%퇴화%토양미생물%토양양분
土壤养分和土壤微生物生长代谢水平的衰退是热带山地退化的重要表现形式,二者的变化基本是一致的,即从热带雨林→33 a次生林→6 a轮歇地→4 a轮歇地→旱谷地→橡胶林→荒草坡呈降低趋势;相对于热带雨林而言,不同利用方式土壤微生物和土壤养分状况均有不同程度的下降,且随退化程度增高减幅增大,土壤微生物衰减的速率比土壤养分的衰减更快。说明山地的退化严重影响着土壤微生物的生长代谢水平以及它们之间的协同作用,从而影响土壤碳氮循环代谢途径,降低土壤肥力水平。
土壤養分和土壤微生物生長代謝水平的衰退是熱帶山地退化的重要錶現形式,二者的變化基本是一緻的,即從熱帶雨林→33 a次生林→6 a輪歇地→4 a輪歇地→旱穀地→橡膠林→荒草坡呈降低趨勢;相對于熱帶雨林而言,不同利用方式土壤微生物和土壤養分狀況均有不同程度的下降,且隨退化程度增高減幅增大,土壤微生物衰減的速率比土壤養分的衰減更快。說明山地的退化嚴重影響著土壤微生物的生長代謝水平以及它們之間的協同作用,從而影響土壤碳氮循環代謝途徑,降低土壤肥力水平。
토양양분화토양미생물생장대사수평적쇠퇴시열대산지퇴화적중요표현형식,이자적변화기본시일치적,즉종열대우림→33 a차생림→6 a륜헐지→4 a륜헐지→한곡지→상효림→황초파정강저추세;상대우열대우림이언,불동이용방식토양미생물화토양양분상황균유불동정도적하강,차수퇴화정도증고감폭증대,토양미생물쇠감적속솔비토양양분적쇠감경쾌。설명산지적퇴화엄중영향착토양미생물적생장대사수평이급타문지간적협동작용,종이영향토양탄담순배대사도경,강저토양비력수평。
The studied area is located at the tropical area in Xishuangbanna where biological diversity is very rich but ecosystem is weak and Swidden agriculture is popular. With population growing, extensive cultivation and overuse of soil resources has resulted soil and environmental degradation, and restricted continuous development of countryside. It is necessary that the study on reason and process of degraded hillslope soil forming.
The swidden system and plantation system are the two main using types in the area. Race land, four years and six years swidden land are different periods in swidden agriculture. Rubber plantation represents an important type of plantation system. Rain forest and wasteland represent original land use and degraded soil respectively, being contrast. The soil samples were collected in September 1997. Microbial quantity, respiration, microbial biomass and nutrient content in the soils were determined, and their variation in soils of different land uses was analysed. The results indicate that the variation pattern of soil microbe is almost same as that of soil nutrient content. The soil microbial quantity, respiration, microbial biomass and nutrient content are all decreased from rain forest→3 years of secondary forest→ix years of swidden land our years of swidden land ace land ubber plantation asteland. The values of soil microbe and nutrient content of different land uses show different degrees of decreasing compared with that of rain forest, and the decreasing extent increased with the increasing degraded extent. It is revealed that the soil microbial growth and metabolism decreased significantly with the increasing of soil degraded extent, and its decreasing speed is rapider than that of soil nutrient. The result show that the change of vegetation and environment and reduce of amount or nutrition of litter fall damage the level of microbial metabolism and nutrient content in soil significantly.
The degradation of soil nutrition and microbial metabolism are the main aspects of tropical land degradation in Xishuanbanna. Burning and cultivating again in short time is an important reason resulting tropical land degradation, at the same time, the soil microbe and nutrient content in plantation are low too. V