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  • CN 62-1070/P
  • ISSN 1000-694X
  • 双月刊 创刊于1981年
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生物与土壤

宁夏盐池沙地3种植物群落土壤表层养分的空间异质性

  • 刘丽丹 ,
  • 谢应忠 ,
  • 邱开阳 ,
  • 时项峰
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  • 宁夏大学 农学院, 宁夏 银川 750021

收稿日期: 2012-04-27

  修回日期: 2012-06-27

  网络出版日期: 2012-06-27

Soil Nutrient Space Heterogeneity in Yanchi of Ningxia Hui Autonomous Region, China

  • LIU Li-dan ,
  • XIE Ying-zhong ,
  • QIU Kai-yang ,
  • SHI xiang-feng
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  • School of Agriculture, Ningxia University, Yinchuan 750021, China

Received date: 2012-04-27

  Revised date: 2012-06-27

  Online published: 2012-06-27

摘要

采用经典统计学和地统计学方法,通过半变异函数及其模型、克里格局部插值估计、空间分布图及分形维数等对宁夏盐池沙地3种植物群落(牛枝子、牛枝子-黑沙蒿、黑沙蒿)土壤表层养分的空间异质性进行了研究。结果表明:0~5 cm土壤有机质、全氮、速效磷含量的空间自相关尺度分别是67 m、519 m、143 m;结构方差比分别为0.558、0.882、0.514,说明结构性因素和随机性因素在0~5 cm土壤有机质和速效磷的空间分布中共同发挥作用。全氮表现出较强空间自相关性,在空间分布上具有明显的结构特征,表明结构性因素在其空间总变异中发挥主导作用。空间格局图反映出0~5 cm土壤有机质、全氮含量表现为牛枝子群落较高,经牛枝子-黑沙蒿群落,含量逐渐减少,至黑沙蒿群落含量又有所增加;0~5 cm土壤速效磷含量表现为牛枝子群落和黑沙蒿群落含量较高而牛枝子-黑沙蒿群落含量较低的趋势。反映出研究区从牛枝子群落经牛枝子-黑沙蒿群落至黑沙蒿群落,植被从以草原种为主的群落,逐渐灌木化,植物群落结构组成由复杂到简单的过程,深刻影响了土壤养分的分布格局,导致了土壤“肥力岛”的形成和发展,又反作用引起研究区植物群落的进一步灌丛化,并逐步向沙漠化的方向发展的趋势。

关键词: 土壤; 养分; 空间异质性

本文引用格式

刘丽丹 , 谢应忠 , 邱开阳 , 时项峰 . 宁夏盐池沙地3种植物群落土壤表层养分的空间异质性[J]. 中国沙漠, 2013 , 33(3) : 782 -787 . DOI: 10.7522/j.issn.1000-694X.2013.00090

Abstract

Using classical statistical and geo-statistical methods such as semivariogram, Kriging interpolation, and spatial distribution maps, we studied the soil nutrient space heterogeneity of Lespedeza potaninii, Lespedeza potaninii-Artemisia ordosica, and Artemisia ordosica community in Yanchi of Ningxia Hui Autonomous Region, which is in arid and semiarid area of China. The results showed that: The autocorrelation scale of soil organic matter, total nitrogen, rapidly-available phosphorus were 67 m, 519 m and 143 m, respectively; Structure variance (C/(Co+C)) were 0.558, 0.882 and 0.514 respectively. The space heterogeneity of total nitrogen content in 0-5 cm soil was mainly influenced by the structural factors, while the organic matter and the available phosphorus contents were influenced by random factors and structural factors. The spatial distribution maps indicated that the organic matter and total nitrogen content in 0-5 cm soil were both the highest in the Lespedeza potaninii community, tapered off in the Lespedeza potaninii-Artemisia ordosica community, and then increased in the Artemisia ordosica community, whereas the available phosphorus content was the highest in the Lespedeza potaninii community and the lowest in the Artemisia ordosica community. In conclusion, the gradual degeneration of the grassland vegetation and the soil desertification had significant influence on the surface soil nutrient distribution pattern when the plant communities converted from Lespedeza potaninii to Artemisia ordosica

参考文献

[1]陈文波,肖笃宁,李秀珍.景观空间分析的特征和主要内容[J].生态学报,2002,22(7):1135-1142.

[2]Robertson G P,Huston M A,Evans F C,et al.Spatial variability in a successional plant community:Patterns of nitrogen availability[J].Ecology,1993,69(5):1517-1524.

[3]张凤杰,乌云娜,杨宝灵,等.呼伦贝尔草原土壤养分与植物群落数量特征的空间异质性[J].西北农业学报,2009,18(2):173-177.

[4]陈防,刘冬碧,熊桂云,等.中亚热带两种水稻土土壤养分空间变异的对比研究[J].土壤学报,2006,43(4):688-692.

[5]秦鱼生,涂仕华,冯文强.成都平原水旱轮作种植下土壤养分特性空间变异研究[J].土壤,2008,45(2):355-359.

[6]金海龙,白祥,满忠龙.新疆艾比湖湿地自然保护区土壤空间异质性研究[J].干旱区资源与环境,2010,24(2):150-157.

[7]毋兆鹏,金海龙.博尔塔拉河、精河流域绿洲土壤空间异质性研究[J].中国沙漠,2010,30(1):120-127.

[8]郭旭东,傅伯杰,陈立顶,等.河北省遵化平原土壤养分的时空变异特征——变异函数与Kriging插值分析[J].地理学报,2000,55(5):555-566.

[9]董国涛,罗格平,许文强,等.三工河流域下游绿洲土壤微量元素有效含量空间变异特征[J].中国沙漠,2010,30(4):862-869.

[10]杨海峰,钱亦兵,蒋超,等.古尔班通古特沙漠南缘主要土壤化学特征的空间异质性[J].中国沙漠,2010,30(2):319-325.

[11]王玉刚,肖笃宁,李彦,等.三工河流域绿洲土壤有机碳的空间分布[J].中国沙漠,2011,31(1):101-107.

[12]郭继勋,祝廷成.羊草草原土壤微生物的数量和生物量[J].生态学报,1997,17(1):78-82.

[13]张晓美,朴春根,李姝江,等.鄂尔多斯南部不同沙地土壤养分含量、酶活性与微生物数量变化规律及其相关性[J].四川农业大学学报,2011,29(3):366-373.

[14]时项锋,许冬梅,邱开阳,等.游动分割窗技术在景观界面影响域判定中的应用——以牛枝子-黑沙蒿群落界面为例[J].草业科学,2010,27(4):30-33.

[15]Lechowicz M J.Caldwell M M.The ecology and genetics of fitness in forest plants.Microspatial heterogeneity of the edaphic environment[J].Journal of Ecology,1991,79(5):687-696.

[16]Robertson G P.Geostatiscs in ecology:Interpolating with known variance[J].Ecology,1987,68(3):744-748.

[17]Schlesinger W H,Reynolds J F,Cunningham G L.Biological feedbacks in global desertification[J].Science,1990,247:1043-1048.

[18]Hook P B,Burke I C,Lanenroth W R.Heterogeneity in soil N and C associated with individual plant sand openings in North American short grass steppe[J].Plant and Soil,1991,138(2):247-256.

[19]郑田,李建贵,李卫红,等.塔里木河下游绿洲荒漠过渡带土壤异质性及对植物群落的影响[J].中国沙漠,2010,30(1):128-134.

[20]Schlesinger W H,Pilmanis A M.Plant-soil interactions in desert[J].Biogeochemistry,1998,42:169-187.

[21]Pickup G.Desertification and climate change:The Australian perspective[J].Climate Research,2003,11:51-63.

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