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

STUDY ON THE SOIL PHYSICOCHEMICAL PROPERTIES OF ZHASHAN IN THE MULI MINING AREA

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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.
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)