ISWC OpenIR  > 水保所知识产出(1956---)
黄土高原粮果生态系统土壤重金属含量变化
李丽霞
学位类型博士
导师郝明德
2008
学位授予单位中国科学院研究生院
学位授予地点陕西
学位专业土壤学
摘要重金属是人类生产生活过程中释放到环境中的主要污染物之一。农药化肥等的施用,污水灌溉、污泥处理等都能增加对农田生态系统土壤重金属的人为输入量。土壤重金属的迁移转化是土壤圈物质循环研究的重要内容之一,本文研究了粮果生态系统土壤重金属的含量变化、形态分级以及迁移转化规律,一方面可丰富生态系统重金属迁移转化理论;另一方面为防止黄土高原土壤环境污染,实现区域经济与生态环境可持续发展,具有重要的理论意义和实际应用价值。所得主要结论如下:1外源微肥与小麦产量、土壤微量元素及重金属的关系1.1施用微肥小麦多年平均增产6%以上,其增产效应在不同降雨年型差异显著。常态年微肥增产机率大于54%,施Cu肥时平均增产13.1%,施BZnMn肥时增产6.3%以上。干旱年施用铜肥和硼肥增产机率为83.3%,小麦分别增产11.8%10.8%;施用锌肥增产5.5%。丰水年施Mn肥平均增产10.5%,施Zn肥平均增产9.3%,增产机率为80%1.2长期施用微肥能增加耕层土壤相应微量元素含量,施铜肥时土壤全Cu增加75.2%有效Cu含量增加5.75施锌肥时土壤有效Zn含量增加3.58倍。施用锰肥时有效Mn含量增加40.1mg/kg。不同微量元素的剖面分布不同, 20-60cm土层有效Cu含量降低,60-100cm含量略有增加;100cm以下土壤有效Cu含量逐渐减少。有效Zn含量在O60cm差异显著,含量随土层加深而迅速下降。土壤有效Mn80cm左右土层有累积现象。1.3长期施用微肥时土壤砷含量降低;土壤汞含量因施肥和土层而异,施Cu肥时0-5cm土层汞含量为0.064mg/kg,降低19.0%5-10cm汞含量为0.606mg/kg,增加1.9倍;10-20cm汞含量为0.369mg/kg,增加3.9倍;Mn肥能增加0-5cm土层汞含量,5-10cm10-20cm土层含量明显下降;施BZnK肥时汞含量降低。土壤镉含量在施ZnMnCu肥时增加3.4%12.1%,施B肥时降低11.8%。土壤铅含量在施用BMnCu肥及K肥时降低8.6%28.9%。土壤铬含量因微肥种类而异。2农田生态系统中的土壤重金属研究2.1小麦连作单施化肥或肥料配施时0-5cm土层汞增加6182%;单施磷肥及肥料配施时5-10cm土层汞含量增加,10-20cm汞含量的变化与5-10cm相似。0-5cm土层砷含量仅在施NP时增加5.9%,单施氮肥或磷肥及肥料配施能增加5-10cm土层砷含量。施NPMNPNPM10-20cm土层砷含量增加,施NMPM时土壤砷含量降低。长期小麦连作不施肥,0-5cm10-20cm土层汞含量较裸地减少36.5%26.0%2.2玉米连作施NPM和轮作施NP肥时,0-5cm土层汞含量分别增加82.7%48.1%5-10cm分别增加18.6%74.4%10-20cm土层汞含量在连作施NPM时降低20%,轮作施NP肥时增加48.0%。玉米连作施NPM0-5cm土层砷含量增加,5-10cm10-20cm砷含量降低;轮作施NP0-5cm5-10cm10-20cm土层砷含量分别较裸地增加47.3%40.5%43.3%2.3豌豆和苜蓿地土壤砷含量增加极显著,苜蓿连作施用NPM 0-5cm5-10cm10-20cm土层砷含量较裸地分别增加29.0%31.3%26.5%;小麦和玉米系统次之。不同作物系统0-5cm土层砷含量增加1.5%41.7%,汞含量在0-5cm土层增加15.4%82.7%5-10cm土层增加4.7%107.0%;在10-20cm土层,苜蓿、玉米系统汞含量分别减少52.0%20.0%,小麦、豌豆系统汞含量分别增加78.0%22.0%,不同土层汞含量差异显著。豌豆和苜蓿系统土壤Cd含量分别增加26.4%8.6%。苜蓿、豌豆、玉米、小麦系统土壤Cr含量分别为70.93mg/kg70.92mg/kg77.30mg/kg77.87mg/kg3果园生态系统的土壤重金属研究3.1土壤铜含量随树龄增加而增加,060cm土层Cu含量增加7%以上;6a果园深层土壤铜含量较高,6a以上果园耕层铜含量较高。果园土壤残渣态铜约占80%,其作物有效性低,在土壤中累积量超过了50kg/hm20-60cm土层潜在可利用态铜的累积量为3040 kg/hm2;可交换态铜的累积量约为10kg/hm2。果园土壤锌含量因树龄而异,26a果园耕层锌含量为114.89mg/kg,较6a果园增加2.43倍,铁锰氧化物态锌超过了56%,残渣态约占35%。果园土壤040cm土层锌的累积量为166.9468.1kg/hm2,作物可利用态锌仅4.714.6kg/hm2,大部分以不可利用态或潜在可利用态存在。3.2土壤Cr含量随树龄线性递增,36a果园Cr含量较6a果园增加17%以上。果园土壤耕层Cr的累积量为100150kg/hm26a15a果园土壤耕层可交换态Cr和铁锰氧物态Cr各占2225%36a果园可交换态Cr1/4,较6龄果园增加58.9%,潜在可利用态Cr6a果园增加51.9%2040cm土壤Cr含量以0.797mg/kg.a的年均增长速率线性增加。4060cm土壤Cr的累积量为110135kg/km2,潜在可利用态铬占5260%15a以上果园较6a果园增加15%以上,36a果园较6a果园增加41.9%。长期种植苹果树能改变土壤可交换态Cr和潜在可利用态Cr的含量和组成。3.3果园土壤Cd含量020cm > 2040cm > 4060cm,随树龄的增加先增加后减少。6a15a36a果园040cm土壤残渣态镉约占70%,其它形态含量较少。26a果园耕层土壤残渣态镉占39.7%、铁锰氧化物态镉占26.9%、可交换态镉占23.8%2040cm土层残渣态镉占51.7%、铁锰氧化物态占25.8%;可交换态占3.5%16.8%4060cm土层,65%以上的镉以残渣态存在于土壤中,铁锰氧化物态占1622%,可交换态小于7%果园生态系统土壤铅含量随树龄按抛物线规律变化;土壤汞、砷含量也随着树龄的增加而变化,15年是果园土壤汞、砷含量变化的转折点,15年前与后,果园土壤汞、砷含量呈现不同的变化趋势。
其他摘要Heavy metals are one of major pollutants which are released to the environment during the process of production and life of human. The application of fertilizers and pesticides, sewage irrigation and sludge treatment and so on can increase the artificial input of the heavy metals to the agro-ecosystem. The migration of heavy metals in the soil is one of the most important contents of the research on material circulating in pedosphere. This article has studied the changes of soil heavy metal content in agriculture and orchard ecosystem as well as their forms and law of migration .On the one hand, it can enrich the theory of heavy metal migration and transformation in ecosystems, on the other hand, It is of great theoretical and practical application value in preventing soil pollution on Loess Plateau and realizing a sustainable development of regional economic and ecological. The main conclusions are as follows:1 Relationship between trace element fertilizer and crop yields, soil microelements and heavy metals1.1 Applying trace element fertilizer for many years, the average yield of wheat increased more than 6%, Effect of trace element fertilizer on yield have great differences depending on the annual precipitation. In a average year, the yield increase probability is bigger than 54%, Applying Cu fertilizer, the yield increased by 13.1%, Applying BZnMn fertilizer, it increased more than 6.3%; In a drought year, yield increase probability is 83.3% when the Cu and B fertilizer supplied, and the yield increased 11.8% and 10.8% separately; Applying Zn fertilizer, it increased 5.5%. In a wet year, Applying Mn fertilizer, the yield increased 10.5%, Applying Zn fertilizer, it increased 9.3%, the increase probability is 80%.1.2 Applying trace element fertilizer for a long time, the corresponding microelements can increase in topsoil, when applied copper fertilizer total-Cu increased by 75.2%, in which available Cu increased 5.75 times. When applied Zn fertilizer, the content of available Zn increased 3.58 times. When applied Mn fertilizer, Available Mn of soil increased 40.1mg/kg. Profile distribution of different microelements is different, Available Cu decreased in the 20-60cm soil layers, and slightly increased in the 60-100cm soil layers; Below 100 cm it reduced gradually. Available Zn in the 0-60cm has a significant difference and it decreased rapidly with the deepening of the soil. Available Mn accumulated in the 80-cm soil layers.1.3 Applying trace element fertilizer for a long time, the soil As content reduced in the soil. The soil Hg content varied depending on fertilization and soil layers. Applying Cu fertilizer, the soil Hg content in 0-5cm layer was 0.064mg/kg,which decreased by 19.0%; in 5-10cm layer it was 0.606mg/kg,which increased 1.9 times; in 10-20cm layer it was 0.369mg/kg, which increased 3.9 times; Mn fertilizer can increase soil Hg content in 0-5 cm layer, it decreased significantly in 5-10 cm and 10-20 cm soil layers; when BZn and K fertilizer supplied, the soil Hg content reduced. Applying ZnMnCu fertilizer, the Cd content of the soil increased 3.4%12.1%, Applying B fertilizer, it decreased 11.8%. Applying BMnCu fertilizer, the soil Pb content decreased 8.6%28.9%. The Cr content of the soil varies due to the trace fertilizer.2. Research on the soil heavy metals in agro-ecosystem2.1 When wheat applied one chemical fertilizer or several fertilizer combined, soil Hg content increased 6.1%~181.8% in 0-5 cm layer; When applying P fertilizer or fertilizer combined, soil Hg increased in 5-10 cm layer; the changes of soil Hg content in 10-20cm are the same as those in 5-10 cm. Soil As content in 0-5 cm layer increased by 5.9% when applying NP only. When applying single N or P fertilizer or combined manure, soil As increased in 5-10cm layer. When applying NPMNPNPM fertilizer, soil As content in 10-20cm layer increased. It decreased when applying NMPM fertilizer. In the control which has no fertilizer supplied, soil Hg content reduced 36.5% and 26.0% obviously contrast to the fallow.2.2 when NPM and NP fertilizer applied in corn continuously, soil Hg contents in 0-5 cm increased 82.7% and 48.1% and it increased 18.6% and 74.4% in 5-10cm layer; Soil Hg content in 10-20cm layer decreased by 20% when applied NPM fertilizer in corn field, and it increased 48.0% when applying NP fertilizer in wheat-corn rotations. Soil As content increased in 0-5cm layer as NPM applied, and it decreased in 5-10cm and 10-20cm layers; Applied NP in the system of wheat-corn rotations, soil As content decreased 47.3%40.5% and 43.3% obviously in 0-5cm5-10cm and10-20cm layers separately.2.3 Cultivated with pea and alfalfa, soil As content increased significantly, when applied NPM in the system of alfalfa continuously, soil As increased 29.0%31.3% and 26.5% obviously in 0-5cm5-10cm and10-20cm layers separately, followed by wheat or corn systems. In different crop systems, As content increased 1.5%41.7% in 0-5cm layer, and its Hg content increased 15.4%82.7% . In 5-10cm layer soil Hg increased by 4.7%107.0%; and in 10- 20cm layer, soil Hg content decreased 52.0% and 20.0% in alfalfa and corn systems separately, and it decreased 78.0% and 22.0% in wheat and pea systems separately. Soil Hg varied distinctly in different soil layers. Soil Cd content increased 26.4% and 8.6% separately in pea and alfalfa system. The soil Cr content were 70.93 mg / kg, 70.92mg/kg, 77.30mg/kg and 77.87 mg / kg when Alfalfa, peas, corn, wheat cultivated.3. Research on soil heavy metals in Orchard ecosystem3.1 Soil Cu content increased with the apple tree age, in 0-60cm layers soil Cu content increased more than 7%; Deep soil Cu content is a high than topsoil in 6 a orchard, but it is higher in topsoil when the was more than 6 years old. Re-Cu are about 80% of the total Cu, which accumulated more than 50 kg/hm2 in the soil and have a low validity. The amount of potential useful Cu cumulated 30-40 kg/hm2 in 0-60cm layer, and the Ex-Cu cumulated about 10 kg/hm2.Soil Zn content is different in Orchard with different ages. Topsoil Zn content is 114.89 mg/kg in a 26 year orchard, increased 2.43 times than that in a 6 year old orchard soil. Ox- Zn is more than 56% of it, Re-Zn is about 35%. The cumulative amount of Zn is 166.9 ~ 468.1 kg/hm2 in 040cm layer, most of which is useless or potential used; Available Zn accumulated 4.714.6kg/hm2.3.2 Soil Cr content increased linearly with ages. The Cr content in 36a orchard increased 17% compared to that in 6a. In topsoil the cumulative amount of Cr reached to 100 ~ 150kg/hm2. Ex- Cr and Ox-Cr are 2225%. Ex-Cr reached to 1/4, increased 58.9% compared to that in 6a orchard. Potential used Cr increased 51.9% compared to that in 6a orchard. In 20-40cm layer, soil Cr content increased linearly in a rate of 0.797 mg / kg.a. In 40-60cm layer, the cumulative amount of Cr is 110135kg/km2. Potential used Cr is 52 ~ 60%, when the orchard was more than 15 years, Potential used Cr increased more than 15%, in 36 years orchard it increased 41.9% compared to 6 years orchard. Planting apple trees for a long time can change the content and composition of Ex-Cr and potential used Cr.3.3 The Cd content of orchard soil:0-20cm > 2040cm > 4060cm, and it decreased after the first increase With the age increasing. Re-Cd is about 70% in 6a, 15a and 36a Orchard. In topsoil of 26a orchard, Re-Cd is 39.7%, Ox-Cd is 26.9%, Ex-Cd is 23.8%; in 20-40cm layer, Re-Cd is 51.7%, Ox-Cd is 25.8% ,and is Ex-Cd is 3.5%16.8%; in 4060cm layer, more than 65% Cd exist in the soil as the form of Re-Cd, Ox-Cd is 1622%,and Ex-Cd is less than 7%; Soil Pb content in orchard eco-system changed with ages according to parabolarule. Soil Hg and As are also changing with the increasing ages, 15 yaer is the turning point of Hg and As content changes in the soil orchard eco-system, the changes of Hg and As in the orchard soil showed different trends before and after 15 years.
文献类型学位论文
条目标识符sbir.nwafu.edu.cn/handle/361005/4079
专题水保所知识产出(1956---)
推荐引用方式
GB/T 7714
李丽霞. 黄土高原粮果生态系统土壤重金属含量变化[D]. 陕西. 中国科学院研究生院,2008.
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