首页|木里矿区渣山土壤理化性质研究

木里矿区渣山土壤理化性质研究

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为了解木里矿区渣山的生态修复区重构土壤理化性质,对土壤养分、土壤含水量、土壤容重、土壤温度及电导率进行了监测.结果表明:①各矿区的土壤养分含量均在中等以上.各矿区的土壤全氮介于1.98~5.32g/kg之间,含量极丰富;除哆嗦贡玛矿区边坡的碱解氮含量较低外,其余均较高,其中聚呼更3号的碱解氮极高,均值达到227.33mg/kg.土壤全磷1.21~1.94g/kg,含量在中上;江仓2号和聚呼更3号的土壤速效磷含量为高或极高,介于25.83~79.20mg/kg之间.土壤全钾含量极高,均大于20.00g/kg;速效钾除哆嗦贡玛为中上外,其余矿区均为极高,介于218.33~581.67mg/kg之间.土壤有机质含量均为极高,介于87.68~205.14g/kg之间.哆嗦贡玛矿区的全磷、速效磷、速效钾和有机质均低于其它矿区,速效磷均值仅为6.58mg/kg、速效钾为148.83mg/kg、有机质为90.87g/kg.②各矿区土壤呈弱碱性.平台的土壤含水量均高于边坡.③各矿区的土壤温度和土壤电导率呈波动性增加,其中,土壤温度在3月8日前均低于0℃,4月30日后高于0℃;土壤电导率在4月30日前较平缓.通过土壤重构,矿区土壤养分状况得到改善.
STUDY ON THE SOIL PHYSICOCHEMICAL PROPERTIES OF ZHASHAN IN THE MULI MINING AREA
To understand the reconstruction of soil physicochemical properties in the ecological restoration area of Zhashan in themulimining area,wemonitored soil nutrients,soilmoisture content,soil bulkdensity,soil temperature,and electrical conductivity.The results indicate that:① The nutrient content of soils in various mining areas is generallymoderate tohigh.The total nitrogen content in the soils ranges from 1.98 to 5.32g/kg,with overall richness.Except for the lower alkali-nitrogen content on the slope of theduosou Gongmamining area,the rest are relatively high,with the alkali-nitrogen content of Polyhymnia 3 reaching an exceptionally high average of 227.33 mg/kg.Total phosphorus in the soil is between 1.21~1.94 g/kg,generally in themedium to high range.The available phosphorus content in Jiangcang 2 and Polyhymnia 3 ishigh or extremelyhigh,ranging from 25.83 to 79.20mg/kg.Total potassium content in the soil is extremelyhigh,all exceeding 20 g/kg,while available potassium,except forduosou Gongma,is extremelyhigh in the othermining areas,ranging from218.33 to581.67mg/kg.Soil organicmatter is extremelyhigh,ranging from 87.68 to205.14 g/kg.Theduosou Gongmamining areahas lower total phosphorus,available phosphorus,available potassium,and organicmatter compared to othermining areas,with average values of 6.58mg/kg,148.83mg/kg,and 90.87 g/kg,respectively.② Soils in allmining areas are weakly alkaline,with platform soilshavinghighermoisture content than slope soils.③ Soil temperature and electrical conductivity in allmining areas show fluctuating increases.Soil temperature remained below 0℃ beforemarch 8 and above 0℃ after April 30,while soil electrical conductivity remained relatively stable before April 30.Soil nutrient status has improved through soil reconstruction in themining area.

Soil physicochemical propertiesMulimining area

土旦加、祁培勇、方伟、史德军、李春英

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青海省草原改良试验站,青海共和 811800

土壤理化性质 木里矿区

2024

青海草业
青海省草原学会 青海省草原总站

青海草业

影响因子:0.316
ISSN:1008-1445
年,卷(期):2024.33(3)