黄土高原果园不同保护性耕作模式土壤水分效应研究
详细信息    本馆镜像全文|  推荐本文 |  |   获取CNKI官网全文
摘要
以洛川为代表的黄土高原中南部地区,因其特有的气候条件和土壤资源,适合优质苹果生产,苹果产业已成为当地发展经济、改善生态环境的支柱产业。但目前当地果园的耕作多采用传统的方式,形成裸露的地表,这样不仅使土壤水分大量蒸发而损失,而且土壤肥力逐年下降,同时由于该地区无补灌措施,且果树生长期间耗水量大,极易导致深层土壤的干燥化,土壤水分不足已制约着当地苹果产业的进一步发展。实践证明,将保护性耕作引入黄土高原果园生产中去,通过少耕、免耕及地表覆盖等综合配套措施,能减少农田土壤水分蒸发,保护农田生态环境,获得生态效益、经济效益和社会效益。
     本研究立足黄土高原果区的资源现状,以最具代表性的苹果园为研究对象,以全年有效抑制果园土壤水分蒸发为目标,系统地对比研究运用免耕、翻耕和旋耕三种耕作方式和生草、覆草、覆膜三种覆盖措施,以及不同耕作和覆盖组合,对黄土高原果园土壤水分、温度、容重和有机质的影响,探索其影响机理;分析单项保护性耕作措施的综合效应,并在此基础上对各种保护性耕作进行整合。主要研究结果如下:
     (1)黄土高原果园随着树龄的增加,土壤各层的水分含量呈逐步下降趋势。1a、5a、10a、15a、20a果园5m平均土壤干燥化指数依次为:133%(无干燥化)、105%(无干燥化)、99%(轻度干燥化)、78%(轻度干燥化)、66%(中度干燥化)。10a果树是果园发生土壤干燥化的界限。20a果园土壤分水在果树4-10月生育期间均表现出较严重的分水亏缺。
     (2)在4-10月果树生长期,不同耕作和覆盖1 m土层蓄水量变化总体趋势相一致,均呈“W”形;各处理在不同的果树生长时期保水效果不同。5月份果园土壤水分临界期不同耕作方式1 m土层土壤水分差异极显著,免耕14.28%﹥旋耕14.13%﹥翻耕13.57%,而在9月份土壤蓄水期其差异并不明显;不同覆盖处理中以覆草处理的土壤水分最高(5月为16.47%,9月为19.42%)且与其他处理差异极显著;在所有耕作和覆盖组合中,免耕覆草保水效果最好且比较稳定,黄土高原果园的保护性耕作体系应以免耕覆草为主。
     (3)生草、覆草、裸地和覆膜5-20 cm各土层昼平均地温覆膜﹥裸地﹥生草﹥覆草;地温昼变幅裸地﹥覆膜﹥生草﹥覆草。7月份各处理之间5-20 cm土层昼平均地温差异和地温变幅都与4月份一致。每个覆盖处理的蓄水量并不是与其地温都成负相关,而是由不同覆盖物的保水效果和保温性质共同决定的。
     (4)黄土高原果园三种不同耕作方式下,20cm土层容重翻耕、旋耕<免耕;不同覆盖处理之间,生草和覆草处理的土壤容重最小且它们之间差异不显著,裸地的土壤容重最大。果园总孔隙度和毛管孔隙度总体呈现出生草>覆草>覆膜>裸地的变化趋势。不同耕作和覆盖措施下土壤水分与容重有一定的负的线性相关关系,但这种相关性并不显著。
     (5)不同耕作方式下黄土高原7月土壤表层有机质免耕﹥旋耕﹥翻耕。不同覆盖处理之间覆草﹥生草﹥覆膜﹥裸地且差异极显著。果实膨大期黄高原果园耕层土壤有机质与1m土层平均土壤水分呈极显著相关关系。
     (6)不同耕作和覆盖措施下土壤容重、温度和有机质对土壤水分的相对重要性按直接通径系数(绝对值)从大到小,依次排列顺序为:有机质(1.0388)>土壤温度(0.5058)>土壤容重(0.2987)。
     本研究结果既能够有效指导提高黄土高原果园土壤水分利用效率,改善果园土壤干燥化状况,又能实现土壤水分生态环境的有效保护和土壤水分资源持续利用,建立科学合理的保护性耕作体系。将为黄土高原地区的果业的进一步发展,农民的持续增收提供坚实的技术保障。
Luochuan which represented in the Loess Plateau in central-southern area, has unique climatic conditions and soil resources, suitable for high-quality apple production. Apple production has become the pillar industries, which development the local economic, and improve ecological environment. However, they also used the traditional farming in orchard production and management, the soil surface is bare, so that not only makes a large number of soil moisture evaporation loss, and an annual decline in soil fertility; There have no irrigation and the fruit trees consume large amount of water during the growth, that’s easily lead to the desiccation of deep soil. Lack water has confined the development of apple industry. Practice has proved that,introduction of conservation tillage in the Loess Plateau orchard production, through less tillage or no-tillage, and mulching, to reduce soil moisture evaporation, protection of agricultural ecological environment, access to eco-efficiency, economic and social benefits .
     This study based on the resources of the Loess Plateau, study the typical apple orchard, to effectively control the orchard soil moisture evaporation in all year, systematically and comparatively study the effects, which used no-tillage, rotary tillage, plow tillage, sod mulch, straw mulch, film mulch and the combination to soil moisture, soil temperature, bulk density and soil organic matter, and explore the mechanism; Analysis and integrated the combined effect of all individual treatment. The main finding follows:
     (1)The soil moisture were gradually declining with the apple tree age increase in Loess Plateau Orchards .The average SDI (soil desiccation index) of 1a, 5a, 10a, 15a, 20a in 5m soil layer were as follows: 133% (without desiccation), 105% (without desiccation), 99% (mild desiccation), 78% (mild dry of), 66% (moderate desiccation). After 10 years the orchard will occur desiccation. 20a Orchard showed a serious deficit of water during apple trees growth.
     (2)During the apple trees growth from April to October, there have the same water storage trend in different tillage and mulching in 1m soil layer, both "W"-shaped; They have different water storage capacity in different growth periods.The difference of different tillage soil moisture was extremely Significant in May in 1m layer, no-tillage 14.28%> rotary tillage 14.13% > plow tillage13.57%; but it was not significant in September; the straw mulch treatment was the higher and extremely significantly soil moisture in all mulching ,was 16.47% in May and 19.42% in September; In all combination of tillage and mulching ,the no tillage- straw mulch have the highest soil moisture and stable, the Loess Plateau orchard conservation tillage system should be based on no tillage- straw mulch.
     (3)The average soil temperature at day in 5cm to 20cm soil layer were that film mulch﹥bare﹥sod mulch﹥straw mulch; The temperature difference at day were that bare﹥film mulch﹥sod mulch﹥straw mulch . It’s similar which average soil temperatures and temperature difference at day between April and July in 5-20cm soil layers in all treatments.It’s not negatively correlated between soil temperature and water storage capacity in all mulch, the soil moisture which in different mulch is the comprehensive results, which effect on soil temperature change, soil moisture hold or consume with mulch.
     (4)The surface soil bulk density in Loess Plateau Orchard was: plow tillage and rotary tillage straw mulch> film mulch > bare. The soil moisture and soil bulk density have a negative correlation in different tillage and mulching, but this correlation is not significant.
     (5)The surface soil organic matter in different tillage in July was that no-tillage﹥rotary tillage﹥plow tillage; the surface soil organic matter in different mulching in July was that straw mulch﹥sod mulch﹥film mulch > bare, and the difference was extremely significant. It was a significant correlation between surface soil organic matter and 1m layer soil moisture in July.
     (6)The arrangement, which the relative importance of soil bulk density, temperature and organic matter for soil moisture in different tillage and mulching, by the direct path coefficient (absolute value) was that organic matter(1.0388)>soil temperature(0.5058)>soil bulk density(0.2987).
     The results of this study is able to effectively improve the Loess Plateau water use, Improve the situation of soil desiccation,Effective protect the ecological environment of soil moisture, Used the soil water resources sustainably and establishment scientific and rational system of conservation tillage. It will provide a solid technical support for fruit industry development in Loess Plateau region and farmers income increase.
引文
[1]李玉山.重新认识黄土高原.水土保持研究[J].1995,12(4).35-42.
    [2]信乃诠,张燕卿,王立祥.中国北方旱区农业研究[M].北京:中国农业出版社,2002.
    [3]孙长忠,黄宝龙,陈海滨,等.黄土高原人工植被与其水分环境相互作用关系研究[J].北京林业大学学报,1998,20 (3):7-14.
    [4]卢宗凡,梁一民,刘国彬.中国黄土高原生态农业[M].西安:陕西科技出版社,1997.31-44.
    [5]高焕文.保护性耕作概念、机理与关键技术[J].四川农机,2005,(4): 22-23.
    [6]杨文治,邵明安.黄土高原土壤水分研究[M].北京:科学出版社,2000,115-117.
    [7]黄明斌,李新民,李玉山.黄土区渭北旱原苹果基地对区域水循环的影响[J].地理学报,2001,56(1):7-13.
    [8]郝淑英刘蝴蝶.黄土高原区果园生草覆盖对土壤物理性状、水分及产量的影响[J],土壤肥料.2003,(1): 23-25.
    [9]张海林,高旺盛,陈阜,等.保护性耕作研究现状、发展趋势及对策[J].中国农业大学学报.2005,10(1):16~20.
    [10] Neil J Southorn. Future directions for dry land soil management under direct seeding techniques-an Australian perspective [C]. Proceedings of 2004 Western States Conservation Tillage Conference,University of California, USA, 2004.
    [11]吴崇友,金诚谦,魏佩敏,等.保护性耕作的本质与发展前景[J].中国农机化,2003,6:8-11.
    [12]李会科,赵政阳,张广军.种植不同牧草对渭北苹果园肥力的影响[J].西北林学院学报, 2004, 19 (2): 31-34.
    [13] Merwin IA, Walke JT. orchard groundcovermanagement impact on soil physical properties [J]. HortScience, 1994, 119 (2): 216-222.
    [14]姚青,朱红惠,陈杰忠.果园柱花草刈割处理对其与柑橘养分竞争的影响[J].园艺学报, 2004, 31 (1): 11-15.
    [15]徐明岗,文石林,高菊生.红壤丘陵区不同种草模式的水土保持效果与生态环境效应[J].水土保持学报, 2001, 15 (1): 77-80.
    [16]朱德兰,吴发启.黄土高原旱地果园土壤水分管理研究[J].水土保持研究,2004,11(1):40-42,115.
    [17]徐呈祥,马艳萍.苹果对水分胁迫的反应特点及节水灌溉研究综述[J].南京农专学报,2000,16(2):15-22.
    [18]樊军,胡波.黄土高原果业发展对区域环境的影响与对策[J].中国农学通报,2005,21(11):355-359.
    [19]李玉山.黄土区土壤水循环特征及其对陆地水文循环的影响[J].生态学报,1983,3(2):91-101.
    [20] Carlos Crovetto Lamarca. Stubble over the soi1 [M].Madison: American Society of Agronomy Inc. 1996.
    [21] Robert D. Grisso. Conservation Tillage [J]. FARM POWER AND MACHINERY, June,1992.
    [22]李国怀、伊华林.生草栽培对柑橘园土壤水分与有效养分及果实产量品质的影响[J].中国生态农业学报,2005,13(2): 161~163.
    [23]张先来,李会科,张广军,等.种植不同牧草对渭北苹果园土壤水分影响的初步研究[J].西北林学院学报,2005,20(3): 56~59.
    [24]陆卫平,陆爱华,陈宗元,等.江苏黄河故道地区苹果园生草及覆盖试验[J].中国南方果树,2006,35(6):6~77.
    [25]杨文治,余存祖.黄土高原区域治理与评价[M].北京:科学出版社,1992.291-294.
    [26]梁一民,李代琼,从心海.吴旗沙打旺草地土壤水分及生产力特征的研究[J].水土保持通报,1990,10(6):113-118.
    [27]侯庆春,韩蕊莲,韩仕峰.黄土高原人工林草地“土壤干层”问题初探[J].中国水土保持,1999,(5):11-14.
    [28]李玉山.黄土高原森林植被对陆地水循环影响的研究[J].自然资源学报, 2001, 16(5): 427-432.
    [29]李军,陈兵,李小芳,等.黄土高原不同植被类型区人工林地深层土壤干燥化效应[J].生态学报.2008,28(4):1441-1445.
    [30]陈云明,刘国彬,杨勤科.黄土高原人工林土壤水分效应的地带性特征[J].自然资源学报, 2004, 19(2): 195-200.
    [31]穆兴民,徐学选,王文龙,等.黄土高原人工林对区域深层土壤水环境的影响[J].土壤学报, 2003, 40(2): 210-217.
    [32]陈洪松,王克林,邵明安.黄土区人工林草植被深层土壤干燥化研究进展.林业科学[J].2005, 41(4): 155-161.
    [33]韩仕峰,李玉山,张孝中,等.黄土高原地区土壤水分区域动态特征[J].中国科学院西北水土保持研究所集刊,1989(10):161-167.
    [34]孙长忠.黄土高原“林分自创性”有效水分供给体系的研究[J].生态学报,1999,19(5):615-621.
    [35]李军,陈兵,李小芳,等.黄土高原不同干旱类型区苜蓿草地深层土壤干燥化效应[J].生态学报.2007,27(1):75-89.
    [36]陈振乾,施明恒.太阳辐射对沙土内部热湿迁移过程影响的实验研究[J].太阳能学报, 1995, (4), 395-400.
    [37]张富仓,张一平.温度对土壤水分保持影响的研究[J].土壤学报, 1997, (2): 160-168.
    [38] Yamanaka T. Yonetani T, Dynamics of the evaporation zone in dry sandy soils [J]. Journal of Hydrology, 1999, 217: 135-148.
    [39] Campbell G S. Soil Physics with Basic: Transport Mod-els for Soil-Plant System [M]. Elsevier, New York, 1985
    [40]姚付启,张振华,钱为君.烟台果园土壤温度影响因素及其预测模型研究[J].农业系统科学与综合研究.2008.24(2):201-204.
    [41] Hogue E.L.,et al. Orchard floor vegetation management. Hort Rev., 1987, (9):377- 430.
    [42] Merwin I.A., et al. Orchard groundcover management impact on apple tree growth and yield, and nutrient availability and uptake. Amer.Soc.Hort.Sci.,1994, 1 19(2):209- 215.
    [43] Tan S.,et al. Competition between perennial ryegrass and'Charclonnay’wine grapes for mineral nutrients. HortScience, 1990, 25(5):533.
    [44]陈伯华.果园人工种草的原则与草种选择,现代农业[J].2003,(6):15.
    [45]张伟,汪春,梁远,等.残茬覆盖对寒地旱作区土壤温度的影响[J].农业工程学报.2006,22(5):71-73.
    [46]冯宝平,张建丰,汪志荣,等.温度对土壤水分运动影响的研究[J].灌溉排水.2001,20(1):45-49.
    [47] Hopmans J W, Dane J H·Temperature dependence of soil water retention curves [J]·Soil Sci Soc Am J,1986, 50:562-56.
    [48] Constantz J, Murphy F·The temperature dependence of ponded infiltration under isothermal conditions [J]·J Hydrol, 1991, 122:119-128·
    [49] Jackson Ray D·Temperature and soil-water diffusivity relation [J]·Soil Sci Soc Am Proc, 1963, 27:363-366·
    [50]冯宝平.入渗条件下温度对土壤水分运动及参数影响的实验研究[M].西安:西安理工大学, 2001.
    [51] Bouyoucos G B·Effect of temperature on the movement ofwater vapor and capillary moisture in soils[J]·JourAgr Res, 1915, 5: 141-172.
    [52] Smith W O. Thermal conductivities in moist soils [J]·Soil Sci Soc Amer Proc, 1940, 4:32-40·
    [53] Gurr C G, Marshall T J, Hutton JT·Movement of water in soil due to a temperature gradient[J].Soil Sci, 1952, 72: 335-344·
    [54]胡定宇.土壤学[M].陕西杨凌:天则出版社,1990.
    [55]王辉,王全九,邵明安.表层土壤容重对黄土坡面养分随径流迁移的影响[J].水土保持学报.2007,21(3):10-13.
    [56]张丹,陈红,高庭艳.生态果园建设对土壤物理特性的影响[J].西南农业学报.2007,20(6):1262-1266.
    [57]刘晚苟,山仑,邓西平.植物对土壤紧实度的反应[J].植物生理学通讯,2001,37(3):254—260.
    [58]曹敏建.耕作学[M].北京:中国农业出版社,2002.
    [59]孙利军,张仁陟,黄高宝.保护性耕作对黄土高原旱地地表土壤理化性状的影响[J].干旱地区农业研究.2007,25(6):207-211.
    [60] Mc Conkey Brian,indwall Wayne.Conservation Tillage Systems in Western Canada[M].北京:中国农业大学出版社, 2000.
    [61]晋凡生,张宝林.旱地玉米农田免耕覆盖的土壤环境效应[J].水土保持研究,2000,7(4):60-64.
    [62] Lal R.No—tillage effects on soil Draperies under differentcrops in Western Nigeria [J].Soil Sci.Soc.Am.J,1976,40(5): 762-768.
    [63]张福武,蔡立群,陈英.免耕对土壤容重总孔隙度和水稳性团聚体的影响[J].甘肃农业科技.2008(8).
    [64]李会科,张广军,赵政阳,等.渭北黄土高原旱地果园生草对土壤物理性质的影响.中国农业科学. 2008,41(7):2070-2076
    [65]雷志栋,杨诗秀,谢森传.土壤水动力学[M].北京:清华大学出版社,1988.77-80.
    [66]康绍忠,粱银丽,蔡焕杰,等.旱区水-土-作物关系及其最优调控原理[M].北京:中国农业出版社,1998.13-24.
    [67]曹崇文,樊贵盛.耕作土壤入渗能力衰减机理[J].太原理工大学学报.2007,38(2):116-118.
    [68]吕殿青,邵明安,刘春平.容重对土壤饱和水分运动参数的影响[J].水土保持学报.2006,20(3):154-157.
    [69]解文艳.土壤结构对土壤入渗能力的影响[J].太原理工大学学报,2004,35(4):381-384.
    [70] Wilding L P,Tessier D.变形土的发生—膨胀收缩现象[J].土壤学进展,1990,18(5):30-36.
    [71]徐建明.土壤有机质.见:黄昌勇主编.土壤学.北京:中国农业出版社,2000.32-49.
    [72]杨景成,韩兴国,黄建辉.土壤有机质对农田管理措施的动态响应[J].生态学报.2003,23(4):788-796.
    [73] Robinson C A, Cruse R M, and Kohler K A. Soil management. In: Hatfield J.L. and Karlen D.L.ed.Sustain-able agriculture systems. Boca Raton, FL: Lewis Publ., 1994. 109-134.
    [74] Kern J S and Johnson M G. Conservation tillage impacts on national soil and atmospheric carbon levels.Soil Sci. Soc.Am.J., 1993,57: 200-210.
    [75] Logan T J, Lal R, and Dick W A. Tillage systems and soil properties in North America.Soil Tillage Research, 1991,20: 241-270.
    [76] Angers D A, Ndayegamiye A and Cote D. Tillage induced difference in organic matter of particle-size fractions and microbial biomass.Soil Sci.Soc.Am.J., 1993,57: 512-516.
    [77] Reicosky D C and Lindstrom K Y. Fall tillage method: Effect on short-term carbon dioxide flux from soil.Agron. J.1993,85: 1237-1243.
    [78] Beare M H, Hendrix P F, and Coleman D C. Water-stable aggregates and organic matter fractions in convention-al-and no-tillage soils.Soil Sci.Soc.Am.J., 1994,58: 777-786.
    [79] Jastrow J D. Soil aggregate formation and the accrual of particulate and mineral associated organic matter.Soil Biol.Biochem.1996,28: 656-676.
    [80]籍增顺,张树梅,等.旱地玉米免耕系统土壤养分研究Ⅰ土壤有机质、酶及氮变化[J].华北农学报, 1998, 13(2): 42-47.
    [81] BlevinsR.L,ThomasG.W, SmithM. S, eta.l Changes in soilprop-erties after 10 years continuous non-tilled and conventionally tilledcom [J]. Soil and Tillage Research, 1983, (3): 135-146.
    [82]逄蕾,黄高宝.不同耕作措施对旱地土壤有机碳转化的影响[J].水土保持学报, 2006, 20: 110-113.
    [83] RachidMrabet,Najib Saber,Azeddine El-Brahl,i eta.l Tota,l partic-ulate organicmatterand structural stability ofaCalcixeroll soilunderdifferentwheat rotations and tillage systems in a semiarid area ofMo-rocco[J]. Soil and Tillage Research, 2001, 57(4): 225-235.
    [84]杨学明,张晓平,方华军,等.北美保护性耕作及对中国的意义[J].应用生态学报, 2004, 15(2): 335-340.
    [85]赵四申,段汝浩,宁吉洲,等.玉米秸秆整株深埋还田技术研究[J].农业工程学报, 2002, 18(2): 58-61.
    [86]高云超,朱文珊,陈文新.秸秆覆盖免耕土壤微生物生物量与养分转化的研究[J].中国农业科学, 1994, 27(6): 41-49.
    [87]张志国,徐琪, BlevinsR.L.长期免耕覆盖对土壤某些理化性质及玉米产量的影响[J].土壤学报, 1998, 35(3): 384-391.
    [88] Hendrix, P. F.,Han, et a.l Soil respiration in conventional and no-tillage agroecosystems under different winter cover crop rotations [J]. Soil and Tillage Research, 1998(12): 135-148.
    [89]孙海国.保护性耕作和植物残体对土壤养分状况的影响[J].中国生态农报, 1997, 1
    [90]李发林,黄炎和,刘长全,等.土壤管理模式对幼龄果园根际土壤养分和酶活性的影响[J].福建农业学报,2002,17(2):112-115.
    [91]李华,惠竹梅,张振文,等.行间生草对葡萄园土壤肥力和葡萄叶片养分的影响[J].农业工程学报, 2004,20(增刊):116-119.
    [92]刘长全,曹明华,傅金辉.红壤幼龄果园土壤肥力变化的综合评价[J].福建热作科技通2000,25(2): 1-7.
    [93]刘蝴蝶,郝淑英,曹琴,等.生草覆盖寸果园土壤养分、果实产量及品质的影响[J].土壤通报,2003,34 (3):184-186.
    [94]章家恩,段舜山,骆世明,等.赤红壤坡地幼龄果园间种不同牧草的生态环境效应[J].土壤与环境,2000,9(1):42-44.
    [95]王彦辉,RADE P.环境因子对挪威云杉林土壤有机质分解过程中重量和碳的气态损失影响及模型[J].生态学报,1999,19(5):641-646.
    [96]王丽莉.温度和水分对土壤腐殖质形成与转化的影响[D].吉林:吉林农业大学,2003.
    [97]黄东迈,朱培立.旱地和水田有机碳分解速率的探讨与质疑[J].土壤学报,1998,35(4):482-491.
    [98] Oliver C D,William R H.Decomposition of rice straw and microbial carbon use efficiency under different soil temperatures and moistures[J].Soil Biology and Biochemistry,2000,32(11-12):1773-1785.
    [99]王力,邵明安,侯庆春.土壤干层量化指标初探[J].水土保持学报.2000,14(4):87-90.
    [100]李会科,赵政阳.果园生草的理论与实践以黄土高原南部苹果园生草实践为例[J].草叶科学,2005(8):32-36.
    [101]刘贤赵,朱孝玉.陕西渭北旱塬苹果种植分区土壤水分特征研究[J].干旱区地理,2004(3):320-324.
    [102] Gardner WR·Solution of the flow equation forthe drying of soils and the porous media[J]·Soil Sci Soc Am Proc, 1959, 23:183-187
    [103] Philip J R·The theory of infiltration: 4·sorptivity and algebraic infiltration equations[J]·Soil Sci, 1957, 84:257-264.
    [104]王国栋,张一平,张君常,等.土壤水势温度滞后效应的研究[J].水土保持研究, 1996, 3(3): 125-130.
    [105]同延安.土壤-植物-大气连续体中水运移理论与方法[M].西安:陕西科技出版社, 1989. 82-83.
    [106]杨金忠,蔡树英.土壤中水、汽、热运动的耦合模型和蒸发模拟[J].武汉水利电力学院学报, 1989, 22(4): 35-44.
    [107]苏衍涛,王凯荣,刘迎新,等.稻草覆盖对红壤旱地土壤温度和水分的调控效应[J].农业环境科学学报,2008(2):670-676.
    [108]冯宝平,张展羽,等.温度对土壤水分运动影响的研究进展[J].水科学进展,2002(5):643-648.
    [109]刘炳成,刘伟,李庆领.温度效应对非饱和土壤中湿分迁移影响的实验[J].华中科技大学学报,2006(4):106-108.
    [110] Sauer T J,Hatfield J L,Prueger J H,et al.Surface energy balance of acorn residue-covered field[J].Agricultural and Forest Meteorology, 1998,89:155-168.
    [111]杨洪强,束怀瑞.苹果根系研究[M],科学出版社,2007:127、145.
    [112]范爱武,刘伟,王崇琦.土壤温度和水分日变化实验[J].太阳能学报,2002(6):721-724.
    [113] Cook H F,Valdes GSB,Lee H C.Mulch effects on rainfall interception, soil physical characteristics and temperature under Zea mays [J].Soil&Tillage Research,2006,91:227-235.
    [114]杜新艳,杨路华,脱云飞,等.秸秆覆盖对夏玉米农田水分状况、土壤温度及生长发育的影响[A].中国农业工程学会2005年学术年会.广州:华南农业大学出版社,2005.213-215.
    [115]吴婕,朱钟麟,郑家国.秸秆覆盖还田对土壤理化性质及作物产量的影响[J].西南农业学报.2006,19(2):192-195.
    [116]邹良栋.植物生长与环境[M].北京:高教教育出版社, 2004, 152-154.
    [117]黄昌勇.土壤学[M].中国农业出版社,北京,2000:89-90.
    [118]郑丽萍,徐海芳.犁底层土壤入渗参数的空间变异性[J].地下水.2006,28(5):55-56
    [119]陈明霞,查轩,丁光敏.翻耕对花岗岩坡地水分转化及产流产沙特征影响研究[J].水土保持通报,2005,25(3):6-9.
    [120]罗奥,崔红秋,杨富江,等.不同耕法的土壤理化及农艺学效应研究进展[J].黑龙江八一农垦大学学报.2008,20(3):34-36.
    [121]雷金银,吴发启,马番.毛乌素沙地南缘保护性耕作措施对土壤物理性质的影响[J].干旱地区农业研究.2008,26(3):161-166.
    [122]张俊华,常庆瑞,贾科利,等.黄土高原植被恢复对土壤肥力质量的影响研究[J].水土保持学报,2003,17(4):38-41.
    [123]田积莹,黄义端.子午岭连家砭地区土壤物理性质与土壤抗侵蚀性能指标的初步研究[J].土壤学报,1964,12(3):278-296.
    [124]刘国彬.黄土高原草地植被恢复与土壤抗冲性形成过程Ⅲ.植被恢复对土壤腐殖质物质及水稳性团聚体的影响[J].水土保持研究,1997, 4(5):122-128.
    [125]田慎重,李增嘉,宁堂原,等.保护性耕作对农田土壤不同养分形态的影响[J].青岛农业大学学报(自然科学版). 2008,25(3): 171-176.
    [126]杨世琦,张爱平,杨正礼,等.黄土高原果园土壤有机质变化趋势分析[J].水土保持研究.2009,16(1):27-31.
    [127] ]DickW. A. Organic carbon, nitrogen, and phosphorus concentra-tions and pH in soil profiles as affected tillage intensity [ J]. Soil Science Society, 1983, 47: 102-107.
    [128]潘伟彬.果园生草对土壤肥力的影响[J].闽西职业技术学院学报.2007,9(2):15-19.
    [129] Campbell C A, McConkey B G, Zentner R P,et al. Long-term effects of tillage and rotations on soil organic Cand total N in a clay soil in southwestern Saskatchewan.Can.J.Soil Sci., 1996,76: 395-401.
    [130]刘思春,吕家珑,马爱生.有机质对黄善土持水性与水肥效应的影响[J].干旱地区农业研究.2005,23(3):65-67.
    [131]艾海舰.土壤持水性及孔性的影响因素[J].干旱地区农业研究. 2002,(3):75-77.
    [132]赵益新.论多元因素统计分析在兽医科研中的应用[J].西南民族学院学报:自然科学版, 1990, 16(1): 101-106.
    [133]明道绪.通径分析[M].雅安:四川农业大学出版社,1990.
    [134] Bhatt GM. Significance of path coefficient analysis in association[J].Euphytica, 1973, 22(2):338-343.
    [135]赵益新,欧阳熙,陈智华,等.动物品种优序决策的多层次模糊数学综合评判[J].四川师范大学学报:自然科学版, 2003, 26(6): 634-635.
    [136]郑彤,陈春云.环境系统数学模型[M].北京:化学工业出版社, 2003.
    [137]殷淑燕,黄春长.黄土高原苹果基地土壤干燥化原因及其对策[J].干旱区资源与环境.2005,19(2):76-79.
    [138]杨维西.试论我国北方地区人工植被的土壤干化问题[J].林业科学,1996,32(1):78-85.
    [139]王克勤,王斌瑞.集水造林防止人工林植被土壤干化的初步研究[J].林业科学,1998,34(4):14-21.
    [140]侯庆春,韩蕊莲,李宏平.关于黄土丘陵典型地区植被建设中有关问题的研究:乡土树种在造林中的意义[J].水土保持研究,2000,7(2):119-123.
    [141]网络.洛川苹果. http://baike.baidu.com/view/1166939.htm.
    [142]彭文英.免耕措施对土壤水分及利用效率的影响[J].土壤通报.2007,38(2):381-383.
    [143]王政友.土壤水分蒸发的影响因素分析[J].山西水利.2003(2):26-27.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700