建瓯市毛竹林土壤基本性质调查研究
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摘要
系统全面调查建瓯市毛竹林土壤背景数据,将有助于毛竹林的科学合理推荐施肥,并能为当地毛竹培育及可持续生产提供依据。本研究通过GPS定位及结合不同乡镇的毛竹林面积,确定全市共计212个样点。在每个采样点,随机采集三个小样混合组成,每个样点按0-20,20-40,40-60cm采集。土壤样品在实验室进行风干过筛。我们分析了土壤样品的不同指标,包括土壤容重、砾石、有机质、全氮、全磷、全钾、有效氮、有效磷、有效钾、pH以及铜、锌、铁、锰等金属元素含量,并运用普通统计学、地统计学及地理信息系统对土壤性质特点及其空间分布特征进行了分析。
     结果表明:(1)建瓯全市毛竹林土壤有机质平均含量在0-20、20-40及40-60cm中分别为3.98%、2.74%与2.13%,高于农田土壤,有机质含量随土壤深度而下降;(2)土壤全氮含量分别为1.48 g/kg、1.06 g/kg及0.87 g/kg,普遍较高,土壤氮与有机质有较好的相关性;(3)土壤全磷分别为2.48g/kg、2.31g/kg及2.58g/kg,含量中等;土壤全钾为19.09、20.10与20.03g/kg;(4)速效氮分别为165.0mg/kg、125.8mg/kg及95.1mg/kg,含量较高,高于当地农田土壤平均值;土壤速效氮与全氮有很好的相关性;(5)土壤中速效磷含量分别为11.37mg/kg、6.90mg/kg及5.83mg/kg,含量低,低于农田土壤;速效磷与全磷无相关性;(6)土壤中速效钾含量分别为54.5mg/kg、46.1mg/kg及49.5mg/kg,较低;速效钾与全钾无相关性;(7)土壤pH平均为4.96,所有土壤样品的pH都在4.5-7.0范围内,适宜于毛竹生长;(8)土壤CEC分别为3.90 cmol/kg、3.81 cmol/kg及3.74 cmol/kg,数值较低;(9)土壤中钠含量高,钙镁含量低,土壤盐基饱和度普遍较低,三层分别为26.7、21.7与19.7%;(10)土壤铜含量一般,分别为34.8mg/kg、38.5mg/kg及41.0mg/kg;锌含量分别为162.7mg/kg、166.8mg/kg及170.1mg/kg;全铁量为46.0 g/kg、48.7 g/kg及49.2 g/kg;锰含量分别为580.5mg/kg、545.8mg/kg及563.4mg/kg;(11)土壤容重一般,分别为0.96 g/cm~3、1.01 g/cm~3及1.03 g/cm~3;土壤中砾石比率比较高,分别为19.1%、20.8%与20.4%。由于地形复杂,建瓯市毛竹林土壤不同元素及成份在地理空间上的分布均存在较大的异质性,差异较大,并且各元素分布并无一致性。
     总的来看,建瓯毛竹林土壤是有机质含量高,富氮低磷缺钾钙镁,pH值适中。建议在强度经营的毛竹林中增施磷钾肥。
In order to provide evidences for moso-bamboo fertilization and the sustainable bamboo production, it is necessary to investigate the bamboo soil basic properties systematically. In this project, GPS was used for the soil sampling site location and the area of bamboo in various towns was considered. According to the towns of Jian’ou city, there were total 212 sample sites selected. Each sample site contained 3 sub-sample sites and soil samples were mixed with the 3 sub-samples. Each soil pedon was done in 3 layers as 0-20, 20-40 and 40-60 cm, respectively. Soil samples were air-dried and sieved in the laboratory. Indicators of soil were included as soil bulk density, organic matter, total nitrogen, total phosphorus, total potassium, available nitrogen, available phosphorus, available potassium, pH, Zn, Cu, Fe and Mn. The common statistics, geo-statistics and geographical information system methods were employed to analyze the spatial distribution characteristics of bamboo soil properties in Jian’ou city.
     The results showed that: (a) Soil organic matter are high as 3.98, 2.74 and 2.13%, respectively, in the three soil layers of 0-20, 20-40 and 40-60cm in the bamboo fields of Jiang’ou city. (b) Soil total nitrogen content is 1.48, 1.06 and 0.87 g/kg, respectively, in the three soil layers that is also higher than that in the local agricultural soil. (c) Soil total phosphorus and potassium content is common as 2.48 and 19.1 g/kg in the surface layer. Bit more is in the next layers. (d) Soil available nitrogen is higher than that in the local agricultural field, its average values are 165.0, 125.8 and 95.1 mg/kg, respectively. (e) Soil available phosphorus content is lower as 11.37, 6.90 and 5.83 mg/kg in the three layers. The content of available phosphorus is not related to the total phosphorus. (f) Soil available potassium content is 54.5, 46.1 and 49.5 mg/kg, respectively, in the 3 different layers. That is also lower and not related to the soil total potassium yet. (g) Soil pH falls in the range of 4.5 to 7.0. That is suitable for the growth of moso-bamboo. (h) Soil CEC is low as 3.90, 3.81 and 3.74 cmol/kg. (i) Low exchangeable cations of Na, Ca and Mg are observed. The base saturation rate is also low as 26.7, 21.7 and 19.7%. (j) Soil copper content is 34.8, 38.5 and 41.0 mg/kg, zinc content is 162.7, 166.8, 170.1 mg/kg, iron content is 46.0, 48.7 and 49.2 g/kg, manganese content is 580.5, 545.8 and 563.4 mg/kg. (k) Soil bulk density is 0.96, 1.01 and 1.03 g/cm~3, the rate of gravel is 19.1, 20.8 and 20.4%. Due to the complicated landform of Jian’ou city, the elements of bamboo soil show great variations in spatial distribution, and various elements are not consistent in distribution.
     Overall, the moso-bamboo soils of Jian’ou city has a high content in organic carbon and nitrogen, but low in phosphorus, and is lack of exchangeable potassium, calcium and magnesium. The soil pH is medium and suitable for moso-bamboo. We suggest that phosphorus and potassium fertilizer should be applied in advance to the intensive managed moso-bamboo field.
引文
[1]祖康祺.土壤[M].北京:科学普及出版社,1986.
    [2]曹志洪.继承传统土壤学成果,促进现代土壤学的发展-论“土壤质量演变规律与可持续利用”研究[J].中国基础科学,2000(10):11-16.
    [3] Blum-Kulka, S. 1989. Playing it safe the role of conventiontionality in indirectness [A]. In S. Blum-Kulka et al (eds.). Cross-culture Pragmatics: Requests and Apologies[C]. Alex Publishing Corporation.
    [4] DORAN JW, PARKIN TB., 1994, Defining and assessing soil quality. In: DORAN J W, COLEMAN D C, BEZDICEK D F,BEZDICEK, AND B.A. STEWART(eds.), Defining soil quality for a sustainable environment. SSSA Spec. Publ.35, Am. Soc. Agron., Madison, WI, pp.3-21.
    [5]林葆,林继雄,李家康.长期施肥的作物产量和土壤肥力的变化[J].植物营养与肥料学报,1994,试刊(1):6-18.
    [6]李忠佩,唐永良,石华,高坤林.不同施肥制度下红壤稻田的养分循环与平衡规律[J].中国农业科学,1998,31:46-54.
    [7]黄耀.中国农田土壤有机变化—基于Meta-分析和模型研究,农田土壤(氮)循环与全球环境变化研究领域前沿战略研讨会[C].南京,2006(6):28-30.
    [8] Andrews, P.D., Y. Ovechkina, N. Morrice, M. Wagenbach, K. Duncan, L. Wordeman, and J.R. Swedlow. 2004. Aurora B regulates MCAK at the mitotic centromere. Dev. Cell. 6:253-268.
    [9] SPARLING, G. P., SCHIPPER, L. A., BETTJEMAN, W. AND HILL.R. 2004. Soil quality monitoring in New Zealand : practical lessons from a 6 -year trial[J]. Agriculture, Ecosystems and Environment, 2004, 104 : 523-534.
    [10]刘世梁,傅伯杰,刘国华,马克明.我国土壤质量及其评价研究的进展[J].土壤通报,2006,37:137-14.
    [11] HAYNES, R.J. Labile organic matter fractions as central components of the quality of agricultural soils: An overview[M]. South Africa, Discipline of Soil Science, 2005.
    [12]唐近春.全国第二次土壤普查与土壤肥料科学的发展[J].土壤学报,1989,26(3):234-239.
    [13]徐昌棠,科学施肥[J].中国林业,1989(9):41.
    [14]张夫道.1996,长期施肥条件下土壤养分的动态和平衡Ⅱ.对土壤氮的有效性和腐殖质氮组成的影响[J].植物营养与肥料学报,2:39-48.
    [15]张爱君,张明普.长期施用有机和无机肥料对黄潮土有机质含量及组成的影响[J].江苏农业研究,2001,22(3):30-33.
    [16] RASMUSSEN, P.E, ROHDE, C.R. 1988. Long-term tillage and nitrogen fertilization effects on organic nitrogen and carbon in semiarid soil[J]. Soil Sci. Soc. Amer. J. 52 (4): 1114-1117.
    [17]李世清,王瑞军,李紫燕,李凤民,邵明安,李生秀.半干旱半湿润农田生态系统不可忽视的土壤氮库-土壤剖面中累积的硝态氮[J].干旱地区农业研究,22,1-13.
    [18] BALLESTA, A.L., IOVERAS, J. 1996. Effects of nitrogen fertilization on maize production and soil nitrate accumulation in the irrigated areas of Ebro Valley (Spain) [A]. Congr. Eur. Soc. For Agron, 4th, Abstracts [C]. The Netherland: Veldhoven, Eur. Soc. for Agron. Wageningen, 1996. 328-329.
    [19]杨伟真,吴明,陈双林.人工经营竹林生态效益发挥与维护研究述评[J].竹子研究汇刊,2003,22 (2):41-43.
    [20]陈存及,吴卫江,杨章儒.毛竹林施用双氰胺渣肥试验研究[J].竹子研究汇刊,1994,13 (2):45-55.
    [21]安黔宁,王建平,胡晓琼.毛竹施肥试验研究.林业杂志[J],1995 (2):1-7.
    [22]陈金林,张献义,叶长青,梁文焰,张碧松,李启鹏.毛竹林高产施肥技术探讨[J].林业科学研究,1996,9(3):323-327.
    [23]戴启惠,黄大勇.粉单竹源浆林施肥制度研究[J].广西林业科学,1997,26 (1):30-34.
    [24]陈雄俊,李贻铨,杨承栋.中国林木施肥与营养诊断研究现状[J].世界林业研究,1998,8 (3):58-65.
    [25]陈立新.人工林土壤质量演变与调控[M].北京:科学出版社,2004.
    [26]高志勤,傅懋毅.不同毛竹林土壤氮养分的季节变化特征[J].浙江林学院学报,2006,23(3):248-254.
    [27]方伟,金爱武,余学军,高培军,桂仁意.竹子现代科技园区综合经营体系建设[J].竹子研究汇刊,2005,24(1):14-18.
    [28]何元荪,何晓东,董水.毛竹春笋高产高效技术[J].浙江林业科技,1998,18 (5):31-38.
    [29]郭晓敏,牛德奎,郭熙,陈防,张过师,张斌,胡冬南.奉新毛竹林土壤养分空间变异性研究[J].植物营养与肥料学报,2006,12(3):420-425.
    [30]郑郁善,陈礼光,洪伟.毛竹杉木混交林生产力和土壤性状研究[J].林业科学,1998,34:16-24.
    [31]彭九生,黄小春,程平.江西毛竹林土壤肥力变化规律初探[J].世界竹藤通讯,2003,1(4):37-42.
    [32]徐秋芳,刘力,洪月明.高低产毛竹林地土壤酶活性比较分析[J].竹子研究汇刊,1998,17(3):37-40.
    [33]徐秋芳,俞益武,钱新标,吴家森.湖州市材用笋用毛竹林土壤理化性质比较分析[J].浙江林学院学报,2003,20(1):102-105.
    [34]楼一平,吴良如,邵大方.毛竹纯林长期经营对林地土壤肥力的影响[J].林业科学研究,1997,10(2):125-129.
    [35] JUNGK A AND CLAASSEN N.Availability in soil and acquisition by plants as the basis forphosphorus and potassium supply to plants[J]. Z P Flanzenernaer Bodenk, 1989, 152:151-157.
    [36]高志勤,傅懋毅.不同毛竹林土壤水分物理性质的特征比较[J].林业科技开发,2005,19(6):12-15.
    [37]蒋文伟,余树全,周国模,姜志林,盛文明.安吉地区不同森林植被水源涵养功能的研究[J];江西农业大学学报(自然科学版);2002,5:71-74.
    [38]王政权.森林土壤化学元素与环境因子关系的研究.东北林业大学学报[J],1989,17(5):20-25.
    [39]周建美.三要素施肥与笋用毛竹林产量构成因子的相关分析[J].竹类研究,1988 (3):21-28.
    [40]周东雄,卢健,张清.毛竹林不同施肥方式比较[J].福建林业科技,1997,74 (3):32-35.
    [41]俞元春,赵永艳,曾曙才.苏南丘陵不同林分类型土壤养分的动态特性[J].浙江林学院学报,1998,15(1):32-36.
    [42]李正才,傅懋毅,谢锦忠.毛竹竹阔混交林群落地力保持研究[J].竹子研究汇刊,2003,22(1):32-37.
    [43]曾曙才,俞元春,徐锦才.枫树山林场不同林分类型土壤养分状况[J].江西林业科技,1997,3:27-29.
    [44]郭晓敏,牛德奎,杜天真,肖冬平,陈防,王婷,彭桂群,雷俊,叶学华.毛竹林平衡施肥持续效应研究初报[J].江西农业大学学报(自然科学版),2002,24(6).
    [45]高雪松,邓良基,张世熔.不同利用方式与坡位土壤物理性质及养分特征分析[J].水土保持学报,2005,19(2):53-56.
    [46]郭旭东,傅伯杰.基于GIS和地统计学的土壤养分空间变异特征研究[J].应用生态学报, 2000,11(4):555-563.
    [47]姜城.不同经营体制下土壤养分空间变异规律及管理技术的研究[D].博士学位论文,2000.
    [48] DAWSON CJ, JOHNSTON AE. Aspects of soil fertility in the interpretation of yield maps as an aid to precision farming [M]. Stafford, JV (Ed.), Precision Agriculture, 1997.
    [49] MALO DD AND WORCESTER BK. Soil fertility and crop responses at selected landscape positions[J]. A Qron. J., 1975, 67:379-401.
    [50]黄承才.浙江省毛竹(Phyllostachys pubescens)林和茶(Camellia sinensis)园土壤库的研究[J].绍兴文理学院学报,2001,21(1):55-57.
    [51]朱元洪.施肥和土壤养分对毛竹笋营养成分的影响[J].土壤学报,1991,28 (1):40-48.
    [52]徐秋芳,姜培坤.毛竹林地土壤养分动态研究[J].竹子研究汇刊,2000,19 (4):46-50.
    [53]金爱武,黄宝龙.参与式技术发展在毛竹笋用林施肥管理中的应用[J].南京林业大学学报(自然科学版),2005,29(4):87-90.
    [54] BAULE H. The fertillzer treatment of forest trees[J]. BLV Verlag, munich. 1970.
    [55]李贻铨.林木施肥与营养诊断[J].林业科学,1991,27(4):435-442.
    [56]周芳纯.竹林培育学[M].北京:中国林业出版社,1998.
    [57]李世东,许传德.中国竹业发展历程与21世纪发展战略[J].竹子研究汇刊,1998,17(1):1-5.
    [58]邱尔发,郑郁善,洪伟.竹林施肥研究现状及探讨[J].江西农业大学学报,2001,23(4):551-555.
    [59]孙培金,杨士德.早竹笋用林施肥效益的分析:不同有机肥配合、硅肥用量、施肥时间的试验效果[J].杭州林业, 1987(1):1-7.
    [60]顾小平,萧江华,梁文焰.毛竹源浆竹林施用氮磷钾肥料效应的研究[J].林业科学,1998, 4(1):25-32.
    [61]楼一平,吴良如,刘耀荣.微肥、激素对竹鞭笋芽萌发的影响[J].林业科学研究,1995,8 (3):322-328.
    [62] PRASAD GK, SINGH SK, DAS PK. Influence of VAM , macro- and micro- nutrients on vegetative propagation of Dendrocalamus strictus[J]. Indian Forestry, 1997 , 123 (9) :863-866.
    [63]汪奎宏,高小辉,潘金贵,吴礼栋,吴菊华,郭人范.毛竹施肥技术经济效果研究[J].竹子研究汇刊,1996, 15(1):21-29.
    [64]黄当亮.毛竹施肥试验研究[J].福建林业科技,1998 (4):27-30.
    [65]戴启惠,黄大勇.丛生竹笋用林施肥试验简报[J].广西林业科学,1996,25 (2):96-99.
    [66]严伍明,杨明亮,胡瑞牯.毛竹笋材两用林配方施肥试验效果初报[J].竹子研究汇报, 1997,16 (4):53-55.
    [67]周国模,吴家森,姜培坤.不同管理模式对毛竹林贮量的影响[J].北京林业大学学报,2006,28(6):51-55.
    [68]黄启堂,陈爱玲,贺军.不同毛竹林林地土壤理化性质特征比较[J].福建林学院学报,2006,26 (4):299-302.
    [69]肖复明,范少辉,汪思龙,熊彩云,张池,刘素萍,张剑.毛竹、杉木人工林生态系统贮量及其分配特征[J].生态学报,2007,27(7):2794-2801.

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