植物生态学报 ›› 2010, Vol. 34 ›› Issue (3): 330-339.DOI: 10.3773/j.issn.1005-264x.2010.03.010 cstr: 32100.14.j.issn.1005-264x.2010.03.010
李军1,2,*(
), 王学春1, 邵明安2, 赵玉娟3, 李小芳1
收稿日期:2009-07-07
接受日期:2009-11-02
出版日期:2010-07-07
发布日期:2010-03-01
作者简介:* E-mail: junli@nwsuaf.edu.cn
LI Jun1,2,*(
), WANG Xue-Chun1, SHAO Ming-An2, ZHAO Yu-Juan3, LI Xiao-Fang1
Received:2009-07-07
Accepted:2009-11-02
Online:2010-07-07
Published:2010-03-01
摘要:
黄土高原人工刺槐(Robinia pseudoacacia)林地深层土壤干燥化现象普遍发生, 日益严峻地威胁着人工植被建设成效。分析和比较半干旱和半湿润地区刺槐林地生物量演变趋势、深层土壤干燥化发生规律和区域分布特征差异, 能够为黄土高原因地制宜地营造刺槐林提供科学依据。在WinEPIC模型气象、土壤和作物参数数据库组建与模拟精度验证的基础上, 应用WinEPIC模型模拟研究了1957-2001年黄土高原半湿润地区洛川和长武、半干旱地区延安和固原等地1-45年生刺槐林地生物量演变规律和深层土壤干燥化效应。结果表明: 洛川、长武、延安和固原的刺槐林地连年净生产力模拟值在5-8年生时达到最大值后, 随着降水量年际波动呈现出明显的波动性降低趋势, 其平均值分别为5.33 × 103、4.56 × 103、4.03 × 103和3.35 × 103kg·hm-2·a-1; 1-7年生刺槐林地年耗水量高于同期年降水量, 导致林地0-10 m土层土壤强烈干燥化, 洛川、长武、延安和固原刺槐林地年均土壤干燥化速率分别为164.3、165.7、187.1和190.0 mm·a-1, 8-45年生刺槐林地有效含水量在0-250 mm的较低水平上随降水量变化而波动; 1-9年生刺槐林地0-10 m土层土壤湿度剖面分布变化剧烈, 土壤湿度逐年降低且土壤干层逐年加厚, 7-9年生时土壤干层厚度已经超过10 m, 8-45年生刺槐林地2-10 m土层土壤湿度保持相对稳定的干燥化状态; 洛川和长武刺槐林地水分生产力较高且相对稳定, 刺槐林地生长期可以超过45年; 而延安和固原刺槐林地水分生产力较低且稳定性差, 刺槐林稳定生长期不超过40年。
李军, 王学春, 邵明安, 赵玉娟, 李小芳. 黄土高原半干旱和半湿润地区刺槐林地生物量与土壤干燥化效应的模拟. 植物生态学报, 2010, 34(3): 330-339. DOI: 10.3773/j.issn.1005-264x.2010.03.010
LI Jun, WANG Xue-Chun, SHAO Ming-An, ZHAO Yu-Juan, LI Xiao-Fang. Simulation of biomass and soil desiccation of Robinia pseudoacacia forestlands on semi-arid and semi-humid regions of China’s Loess Plateau. Chinese Journal of Plant Ecology, 2010, 34(3): 330-339. DOI: 10.3773/j.issn.1005-264x.2010.03.010
图2 各地实测年降水量(A)与模拟的刺槐林地干旱胁迫日数(B)、连年净生产力(C)和生物量(D)的变化。
Fig. 2 Changes of observed annual rainfall (A) and simulated water stress days (B), annual net productivity (C) and biomass (D) of black locust forestlands at four sites.
图4 各地刺槐林地0-10 m土层逐月土壤有效含水量模拟值变化动态。 A, 1-7年生。B, 8-26年生。C, 27-45年生。
Fig. 4 Changes of simulated available soil water content in 0-10 m soil layers on black locust forestlands at four sites. A, 1- to 7-year-old. B, 8- to 26-year-old. C, 27- to 45-year-old.
图6 黄土高原各地不同林龄刺槐林地0-10 m土层土壤湿度剖面分布变化比较。
Fig. 6 Comparison of soil moisture distribution changes in 0-10 m profiles on different stand age black locust forestlands at four sites of the Loess Plateau.
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