不同种植时间脐橙园土壤理化特性研究

张维玲,张金池

南京林业大学学报(自然科学版) ›› 2018, Vol. 42 ›› Issue (04) : 181-186.

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南京林业大学学报(自然科学版) ›› 2018, Vol. 42 ›› Issue (04) : 181-186. DOI: 10.3969/j.issn.1000-2006.201711023
研究简报

不同种植时间脐橙园土壤理化特性研究

  • 张维玲1,2,张金池1*
作者信息 +

Effects of different planting years on soil physical and chemical properties in navel orange orchard

  • ZHANG Weiling1,2,ZHANG Jinchi1*
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文章历史 +

摘要

【目的】通过研究不同种植年限脐橙园土壤理化特性,为脐橙园施肥管理提供理论依据。【方法】以未种植地(对照)、2年生、4年生、9年生、15年生、23年生6个脐橙园为研究对象,采集样点0~20 cm,≥20~40 cm,≥40~60 cm土层土壤,分别测定土样的物理性黏粒含量、容重、20 cm蓄水量、有机质、速效氮、速效磷、速效钾、全氮、全磷含量和pH等土壤理化性质。【结果】脐橙种植年限对土壤容重和蓄水量影响不显著。土层对土壤容重、蓄水量在土层之间存在极显著的影响(P<0.001),随着土层加深,土壤容重和蓄水量逐渐升高。脐橙种植年限、土层及其交互作用对土壤物理性黏粒均存在极显著影响(P<0.001),2年生及4年生果园上层土壤物理性黏粒显著低于未种植对照地(P<0.05),而23年生林地则显著高于未种植对照地(P<0.05),下层土壤物理性黏粒变化无显著规律。脐橙种植年限、土层深度及其交互作用对各土壤化学性质的影响均达到极显著水平(P<0.001),脐橙园中层土壤的pH均显著低于未种植对照地,下层土壤的pH则是随着种植年限的增加而逐渐降低。15年生脐橙园土壤各土层的有机质、速效磷、全氮、全磷含量均显著高于其他年限(P<0.05),上层土壤的速效氮含量在23年生果园达到最高值。土壤有机质、速效氮、速效磷、速效钾、全氮、全磷与土壤物理性黏粒呈正相关关系,而与pH、土壤容重、蓄水量呈负相关关系。【结论】脐橙种植年限对土壤理化特性存在显著影响,随着脐橙种植年限延长,土壤逐渐酸化,表层土壤物理性黏粒含量呈先降低后升高的趋势; 15年生果园土壤总体肥力显著高于其他种植年限。

Abstract

Abstract: 【Objective】The present study investigated the physical and chemical properties of soil in a navel orange orchard from different planting years. This was done to obtain data to form a theoretical basis for making informed fertilization management decisions. 【Method】Six treatments were examined: control plantation(unplanted), and land 2 years, 4 years, 9 years, 15 years and 23 years after planting. Soil samples were collected in each plot at three depths(0-20 cm, ≥20-40 cm and ≥40-60 cm), which were then used for analyses of soil physical and chemical characteristics, including physical clay content, bulk density, 20 cm soil water storage capacity, content of soil organic matter, available nitrogen, available phosphorus, available potassium, total nitrogen as well as total phosphorus, and pH. 【Result】The influence of navel orange planting years on soil volume and water storage was not significant. The soil layer exerted significant effects on soil bulk density and water storage capacity(P < 0.001), both of which increased with the soil layer depth. The navel orange planting years, soil layers and their interactions exerted significant influences on soil physical clay content(P < 0.001). The soil physical clay content of top soil from 2-and 4-year plantations was significantly lower than that of control plantations(P < 0.05). However, the soil physical clay content from 23-year plantations was significantly higher than that of control plantations(P < 0.05). In addition, no obvious trends in differences in subsoil physical clay content among different plantations were found in this study. The navel orange planting years, soil layers, and their interactions had significant influences on soil chemical properties(P < 0.001). The middle layer soil pH in navel orange plantations was significantly lower than that in control plantations, and the subsoil pH decreased as the depth of the soil layer. The content of soil organic matter, available phosphorus, total nitrogen and total phosphorus in 15-year plantations were significantly higher than those in all other plantations(P < 0.05), and the content of available nitrogen was the highest in 23-year plantations. The content of soil organic matter, available nitrogen, available phosphorus, available potassium, total nitrogen, and total phosphorus were positively correlated with physical clay content, and negatively correlated with bulk density, water storage capacity and pH. 【Conclusion】Navel orange plantation age had a profound impact on soil physicochemical properties. Soil pH decreased, and physical clay content of the surface soil first decreased and then increased, with increasing years of planting. Soil fertility of 15-year plantations was significantly higher than that in all other plantations.

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张维玲,张金池. 不同种植时间脐橙园土壤理化特性研究[J]. 南京林业大学学报(自然科学版). 2018, 42(04): 181-186 https://doi.org/10.3969/j.issn.1000-2006.201711023
ZHANG Weiling,ZHANG Jinchi. Effects of different planting years on soil physical and chemical properties in navel orange orchard[J]. JOURNAL OF NANJING FORESTRY UNIVERSITY. 2018, 42(04): 181-186 https://doi.org/10.3969/j.issn.1000-2006.201711023
中图分类号: S714   

参考文献

[1] 郭梅,彭晓春,郑延敏,等.东江源受偿意愿调查与跨省生态补偿机制研究[J].环境科学与技术,2013,36(5): 183-187. DOI:10.3969/j.issn.1003-6504.2013.05.036. GUO M,PENG X C,ZHENG Y M, et al. Ecological compensation in Dongjiang Headwaters based on the survey[J]. Environmental Science & Technology,2013,36(5): 183-187.
[2] 陈亚艳,罗新祜. 赣南脐橙出口特点及竞争力影响因素实证分析[J]. 中国南方果树,2015,44(1): 126-132. DOI:10.13938/j.issn.1007-1431.2015.44.01.039. CHEN Y Y,LUO X H. Gannan navel orange export characteristics and empirical analysis of competitiveness of the influencing factors [J]. Fruit Trees in Southern China,2015,44(1):126-132.
[3] 赖晓桦,黄传龙,谢上海,等. 赣南脐橙施肥情况调查研究[J]. 中国南方果树,2009,38(4): 30-32. DOI:10.13938/j.issn.1007-1431.2009.04.017. LAI X H,HUANG C L,XIE S H,et al. Study on fertilization situation of navel orange in Gannan[J].Fruit Trees in Southern China,2009,38(4): 30-32.
[4] 杨晓娟,王海燕,刘玲东,等. 东北过伐林区不同林分类型土壤肥力质量评价研究[J]. 生态环境学报,2012,21(9): 1553-1560. DOI:10.16258/j.cnki.1674-5906.2012.09.011. YANG X J,WANG H Y,LIU L D,et al. Evaluation of soil fertility quality under different forest stands in over-logged forest region,northeast China [J]. Ecology and Environmental Sciences,2012,21(9): 1553-1560.
[5] 魏彬萌,王益权.渭北果园土壤物理退化特征及其机理研究[J].植物营养与肥料学报,2015,21(3):694-701. DOI:10. 11674 /zwyf.2015. 0316. WEI B M,WANG Y Q. Physical degradation characteristics and mechanism of orchard soil in Weibei Region[J].Journal of Plant Nutrition and Fertilizer,2015,21(3):694-701.
[6] 张玉树,张金波,朱同彬,等.不同种植年限果园土壤有机氮组分变化特征[J].生态学杂志,2015,34(5):1229-1233. DOI:10.13292/j.1000-4890.20150311.001. ZHANG Y S,ZHANG J B,ZHU T B,et al. Characteristics of soil organic nitrogen components of orchards with different planting ages[J]. Chinese Journal of Ecology, 2015,34(5):1229-1233.
[7] 马艳春,姚玉新,杜远鹏,等.葡萄设施栽培不同种植年限土壤理化性质的变化[J].果树学报,2015,32(2):225-231.DOI:10.13925/j.cnki.gsxb.20140203. MA Y C, YAO Y X,DU Y P,et al. Changes of soil physical and chemical properties in different planting years of grape cultivation[J].Journal of Fruit Science,2015,32(2):225-231.
[8] 李树勇,周小江,殷剑敏,等. 寻乌县脐橙种植气候地形土壤综合区划[J]. 江西农业学报,2007(5):40-43. DOI:10.19386/j.cnki.jxnyxb.2007.05.012. LI S Y,ZHOU X J,YIN J M,et al. Climatic terrain soil comprehensive division of navel orange plantation in Xunwu County[J]. Acta Agriculture Jiangxi,2007(5): 40-43.
[9] 刘艳,宋同清,蔡德所,等. 喀斯特峰丛洼地不同土地利用方式土壤肥力特征[J]. 应用生态学报,2014,25(6):1561-1568. DOI:10.13287/j.1001-9332.20140415.004. LIU Y,SONG T Q,CAI D S,et al. Soil fertility characteristics under different land use patterns in depressions between karst hills [J]. Chinese Journal of Applied Ecology. 2014,25(6):1561-1568.
[10] 鲍士旦,土壤农化分析[M]. 3版. 北京: 中国农业出版社 2013: 260-281. BAO S D.Soil agro-chemistrical analysis[M].3rd ed. Beijing: China Agriculture Press,2007:260-281.
[11] 张学权,胡庭兴. 林(竹)草不同植被恢复模式下的土壤物理特性[J]. 长江流域资源与环境,2008(4):623-627.DOI:10.3969/j.issn.1004-8227.2008.04.023. ZHANG X Q,HU T X. Soil physical characteristics under different vegetation restoration patterns of forest(bamboo)grass under different vegetation restoration patterns. [J] Resources and Environment in The Yangtze Basin Resour Environ Yangtze Basin.2008(4):623-627.
[12] 胡敏,向永生,张智,等. 恩施州耕地土壤pH近30年变化特征[J]. 应用生态学报,2017,28(4):1289-1297. DOI:10.13287/j.1001-9332.201704.017. HU M,XIANG Y S,ZHANG Z,et al. Variation characteristics of farmland soil pH in the past 30 years of Enshi Autonomous Prefecture,Hubei,China[J]. Chinese Journal of Applied Ecology,2017,28(4): 1289-1297.
[13] 孙晓,庄舜尧,刘国群,等. 集约经营下雷竹林土壤酸化的初步研究[J]. 土壤通报,2010,41(6):1339-1343. DOI:10.19336/j.cnki.trtb.2010.06.011. SUN X,ZHUANG S Y,LIU G Q,et al. A preliminary study of soil acidification under Lei bamboo plantation with intensive management [J]. Chinese Journal of Soil Science,2010,41(6):1339-1343.
[14] 杨东伟,章明奎. 水田改果园后土壤性质的变化及其特征[J]. 生态学报,2015,35(11):3825-3835. DOI:10.5846/stxb201309212319. YANG D W,ZHANG M K. Effects of land-use change from paddy field to orchard farm on soil property shift processes and their characteristics[J]. Acta Ecologica Sinica,2015,35(11): 3825-3835.
[15] 孙宝伟,杨晓东,张志浩,等. 浙江天童常绿阔叶林演替过程中土壤碳库与植被碳归还的关系[J]. 植物生态学报,2013,37(9):803-810.DOI:10.3724/SP.J.1258.2013.00084. SUN B W,YANG X D,ZHANG Z H,et al. Relationships between soil carbon pool and vegetation carbon return through succession of evergreen broad-leaved forests in Tiantong region,Zhejiang Province,eastern China[J].Chinese Journal of Plant Ecology,2013,37(9):803-810.
[16] 舒正悦,王景燕,龚伟,等. 重合养殖对柑橘林土壤微团聚体分形特征及理化性质的影响[J]. 南京林业大学学报(自然科学版),2017,41(5):92-98. DOI:10.3969/j.issn.1000‐2006.201605004. SHU Z Y,WANG J Y,GONG W,et al. Effects of raising chicken in citrus orchard on soil micro-aggregate fractal feature and soil physical and chemical properties[J]. Journal of Nanjing Forestry University(Natural Sciences Edition),2017,41(5):92-98.
[17] 张秀,张黎明,龙军,等.亚热带耕地土壤酸化程度差异及影响因素[J].中国生态农业学报,2017,25(3):441-450. DOI:10.13930/j.cnki.cjea.160723. ZHANG X,ZHANG L M,LONG J,et al. Soil acidification degree difference and impact factors of subtropical cropland[J]. Chinese Journal of Eco-Agriculture,2017,25(3):441-450.

基金

基金项目:国家林业公益性行业科研专项项目(201504406); 江苏高校优势学科建设工程资助项目(PAPD) 第一作者:张维玲(6115504@qq.com)。*通信作者:张金池(zhang8811@njfu.edu.cn),教授。

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