黑龙江五大连池市卧虎山农场土壤营养元素地球化学特征研究
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摘要
为研究火山岩地区土壤中营养元素的浓度水平及其空间分布特征,选取黑龙江五大连池卧虎山农场为研究区,系统采集41件表层土壤样品,测试分析氮、磷、钾等植物营养元素以及有机质、pH值等15项指标,绘制元素地球化学图,掌握了该区营养元素含量的空间分布特征。根据相关标准,评价土壤中营养元素的丰缺水平。结果表明:(1)研究区为酸性土壤,土壤营养元素含量总体丰足,只有硼含量稍缺或缺乏;(2)土壤营养元素具有明显的空间分布规律,以卧虎山北部含量较高、跃进水库附近较低为特征;(3)研究区为温暖湿润条件下的中等化学风化,伴随着成土作用营养元素持续从岩石释放到土壤中,且有机质对土壤营养元素具有良好的吸附性。本研究为当地农业生产中养分的合理利用和农业种植规划提供了第一手数据资料。
In order to investigate the concentration and spatial distribution,as well as geochemical characteristics of nutrition elements in the volcanic rock area of the Wohushan farm in Wudalianchi,Heilongjiang province,a total of 41 topsoil samples were collected and the concentration of essential nutrient elements and physic-chemical indexes,such as nitrogen,phosphorus,potassium,organic matter as well as pH were measured.The abundance and deficiency level of nutrient elements in soils were evaluated according to the relevant standards. The results show that:( 1) the type of soil in the study area belongs to acidic soil,and the soil nutrient elements of the study area are of high quality,except that boron element content is slightly deficient or lacking;( 2) the spatial distribution of soil nutrient elements,is characterized by a higher value in the north of the Wohushan farm and a lower level near the Yuejin reservoir;( 3) the soil within the study area were deve-loped under the moderate chemical weathering and warm humid conditions. The nutrients were released continuously into the soils in the process of soil forming,and organic matters had good adsorption capacity for soil nutrients.This study provides first-hand data for the rational use of nutrients in the local agricultural production and the planning of agricultural planting.
In order to investigate the concentration and spatial distribution,as well as geochemical characteristics of nutrition elements in the volcanic rock area of the Wohushan farm in Wudalianchi,Heilongjiang province,a total of 41 topsoil samples were collected and the concentration of essential nutrient elements and physic-chemical indexes,such as nitrogen,phosphorus,potassium,organic matter as well as pH were measured.The abundance and deficiency level of nutrient elements in soils were evaluated according to the relevant standards. The results show that:( 1) the type of soil in the study area belongs to acidic soil,and the soil nutrient elements of the study area are of high quality,except that boron element content is slightly deficient or lacking;( 2) the spatial distribution of soil nutrient elements,is characterized by a higher value in the north of the Wohushan farm and a lower level near the Yuejin reservoir;( 3) the soil within the study area were deve-loped under the moderate chemical weathering and warm humid conditions. The nutrients were released continuously into the soils in the process of soil forming,and organic matters had good adsorption capacity for soil nutrients.This study provides first-hand data for the rational use of nutrients in the local agricultural production and the planning of agricultural planting.
引文
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[27]刘颖,魏丹,李玉影.黑龙江省主要类型土壤剖面养分分布研究[J].黑龙江农业科学,2015(11):31-34.
[28]王雅琴,冯君,尹秀英,等.吉林省大豆种植区土壤的机械组成、pH值及营养元素与产量的关系[J].吉林农业大学学报,2004,26(6):653-658.
[29]宋淑娥,金竹.辽河平原表层土壤养分性状和分布特征[J].建筑工程技术与设计,2015(33):1591.
[30] REIMANN C,KASHULINA G,CARITAT P D,et al. Multi-element,multi-medium regional geochemistry in the European Arctic:Element concentration,variation and correlation[J]. Applied Geochemistry,2001,16(7):759-780.
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[32]林万树.古田县果园土壤氮磷钾状况及其与有机质和pH的相关性[J].上海农业学报,2015,31(1):44-48.
[33]章程,谢运球,吕勇,等.广西弄拉峰丛山区土壤有机质与微量营养元素有效态[J].中国岩溶,2006,25(1):63-66.
[34]邓邦良,袁知洋,李真真,等.武功山草甸土壤有效态微量元素与有机质和pH的关系[J].西南农业学报,2016,29(3):647-650.
[2]陆文祥,李明东,魏学铭.黑龙江省五大连池农场大豆优质高产掠影[J].农场经济管理,2016(11):70-71.
[3]赵其国.中国的火山灰土[J].土壤学报,1988,22(4):323-329.
[4]黑龙江省土地管理局.黑龙江土壤[M].北京:农业出版社,1992:326-334.
[5]崔玉军,时永明,刘国栋,等.黑龙江省松嫩平原南部黑土的元素含量特征[J].现代地质,2008,22(6):929-933.
[6]雷国平,代路,宋戈.黑龙江省典型黑土区土壤生态环境质量评价[J].农业工程学报,2009,25(7):243-248.
[7]隋跃宇,张兴义,张少良,等.黑龙江典型县域农田黑土土壤有机质现状分析[J].土壤通报,2008,39(1):186-188.
[8]辛刚,颜丽,汪景宽,等.不同开垦年限黑土有机质变化的研究[J].土壤通报,2002,33(5):332-335.
[9]付嵩,丁玉进,张新远,等.青海省民和县新民—李二堡地区土壤养分地球化学特征分析[J].现代地质,2018,32(5):1103-1108.
[10]张文华.五大连池火山地貌世界地质公园[J].生物学教学,2005,30(5):19-20.
[11]黑龙江省黑河地区科学技术委员会,黑龙江省德都县科学技术委员会.黑龙江省德都五大连池火山地质和矿产资源的综合利用[M].黑河:黑龙江省黑河地区科学技术委员会,1974:9-21.
[12]周志强,徐丽娇,张玉红,等.黑龙江五大连池的生态价值分析[J].生物多样性,2011,19(1):63-70.
[13]杨忠芳,余涛,李敏,等. DZ/T0295—2016.土地质量地球化学评价规范[S].北京:地质出版社,2016:1-52.
[14]刘忠,尚义.植物必需营养元素的来源[J].现代农业,2011(11):28-29.
[15]王忠.植物生理学[M].北京:中国林业出版社,2000:80-89.
[16]唐将,李勇,邓富银,等.三峡库区土壤营养元素分布特征研究[J].土壤学报,2005,42(3):473-478.
[17]顾清,庞海云,丁险峰,等.中量营养元素在农业生产上的应用[J].现代化农业,2006(11):16-18.
[18]吕选忠.元素生物学[M].合肥:中国科学技术大学出版社,2011:238-312.
[19]马扶林,宋理明,王建民.土壤微量元素的研究概述[J].青海科技,2009,16(3):32-36.
[20]马扶林.微量元素对农作物品质影响概述[J].青海草业,2009,18(2):32-35.
[21]汤璐,汤英.中、微量元素对主要农产品品质的影响综述[J].安徽农学通报,2008,14(19):61-63.
[22]李德军,莫江明,方运霆,等.鼎湖山自然保护区不同演替阶段森林土壤中有效微量元素状况研究[J].广西植物,2004,24(6):529-534.
[23]窦森.土壤有机质[M].北京:科学出版社,2010:14-15.
[24]方小满,施雯,李非里,等.溶解性有机质对水中重金属生物有效性的影响研究[J].环境科技,2016,29(2):59-63.
[25]宋刚,胡腾胜.剑河县土壤微量元素与有机质、pH值的关系研究[J].耕作与栽培,2014(3):20-21.
[26]于君宝,王金达,刘景双,等.典型黑土pH值变化对微量元素有效态含量的影响研究[J].水土保持学报,2002,16(2):93-95.
[27]刘颖,魏丹,李玉影.黑龙江省主要类型土壤剖面养分分布研究[J].黑龙江农业科学,2015(11):31-34.
[28]王雅琴,冯君,尹秀英,等.吉林省大豆种植区土壤的机械组成、pH值及营养元素与产量的关系[J].吉林农业大学学报,2004,26(6):653-658.
[29]宋淑娥,金竹.辽河平原表层土壤养分性状和分布特征[J].建筑工程技术与设计,2015(33):1591.
[30] REIMANN C,KASHULINA G,CARITAT P D,et al. Multi-element,multi-medium regional geochemistry in the European Arctic:Element concentration,variation and correlation[J]. Applied Geochemistry,2001,16(7):759-780.
[31] NESBITT H W,YOUNG G M. Early Proterozoic climates and plate motions inferred from major element chemistry of lutites[J]. Nature,1982,299:715-717.
[32]林万树.古田县果园土壤氮磷钾状况及其与有机质和pH的相关性[J].上海农业学报,2015,31(1):44-48.
[33]章程,谢运球,吕勇,等.广西弄拉峰丛山区土壤有机质与微量营养元素有效态[J].中国岩溶,2006,25(1):63-66.
[34]邓邦良,袁知洋,李真真,等.武功山草甸土壤有效态微量元素与有机质和pH的关系[J].西南农业学报,2016,29(3):647-650.
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