植物生态学报 ›› 2013, Vol. 37 ›› Issue (7): 665-673.DOI: 10.3724/SP.J.1258.2013.00069
所属专题: 稳定同位素生态学
收稿日期:
2013-01-05
接受日期:
2013-04-01
出版日期:
2013-01-05
发布日期:
2013-07-05
通讯作者:
郑新军
作者简介:
* E-mail: 基金资助:
ZHOU Hai1,2,*(),ZHENG Xin-Jun1,**(
),TANG Li-Song1,LI Yan1
Received:
2013-01-05
Accepted:
2013-04-01
Online:
2013-01-05
Published:
2013-07-05
Contact:
ZHENG Xin-Jun
摘要:
荒漠生态系统中, 水是植物生长最主要的限制因子。为了比较同一生境下不同荒漠植物的水分来源特征, 选取了同一生境下的多枝柽柳(Tamarix ramosissima)、白刺(Nitraria sibirica)和红砂(Reaumuria soongorica), 测定了这3种植物茎水和各潜在水源(降水、土壤水和地下水)的氢、氧稳定同位素比率(δD和δ18O)值, 并利用IsoSource软件计算了3种植物对潜在水源的利用比例。结果表明: 红砂和白刺的茎水δD和δ18O值及其水分来源有明显的季节波动特征。其中, 红砂为浅根系植物, 春季(3-5月)以表层土壤水为主要水源, 夏秋季节(6-10月)表层土壤含水量显著降低, 其主要的水分来源逐渐偏向于较深层的土壤水; 白刺的根系分布范围介于红砂和多枝柽柳之间, 在春季能够较多地利用表层土壤水, 而到了夏秋季节, 所利用的水分更多地来源于深层土壤水或地下水; 多枝柽柳为深根系植物, 其90%以上的水分来源于深层土壤水和地下水, 而且茎水δD和δ18O值及其水分来源没有季节波动特征。3种植物水分来源特征的差异与其水分利用策略密切相关, 同时, 也说明荒漠灌木可以通过自身调节向着最优(最有利)表现型发展, 从而最大限度地获取水分。
周海,郑新军,唐立松,李彦. 准噶尔盆地东南缘多枝柽柳、白刺和红砂水分来源的异同. 植物生态学报, 2013, 37(7): 665-673. DOI: 10.3724/SP.J.1258.2013.00069
ZHOU Hai,ZHENG Xin-Jun,TANG Li-Song,LI Yan. Differences and similarities between water sources of Tamarix ramosissima, Nitraria sibirica and Reaumuria soongorica in the southeastern Junggar Basin. Chinese Journal of Plant Ecology, 2013, 37(7): 665-673. DOI: 10.3724/SP.J.1258.2013.00069
高度 Height (cm) | 冠幅 Crown diameter (cm) | 根深 Root depth (cm) | 总吸收根表面积 Total surface area of absorbing roots (cm2) | |
---|---|---|---|---|
多枝柽柳 Tamarix ramosissima | 175.0 ± 13.4 | 155.0 ± 17.2 | ≥310 | 30 249.2 ± 34.3 |
白刺 Nitraria sibirica | 78.3 ± 5.8 | 328.6 ±18.36 | ≥200 | 10 622.1 ± 26.4 |
红砂 Reaumuria soongorica | 55.0 ± 8.2 | 35.0 ± 5.6 | 80.0 ± 25.7 | 361.8 ± 19.7 |
表1 多枝柽柳、白刺和红砂灌丛的形态特征
Table 1 Morphological characteristics of Tamarix ramosissima, Nitraria sibirica and Reaumuria soongorica
高度 Height (cm) | 冠幅 Crown diameter (cm) | 根深 Root depth (cm) | 总吸收根表面积 Total surface area of absorbing roots (cm2) | |
---|---|---|---|---|
多枝柽柳 Tamarix ramosissima | 175.0 ± 13.4 | 155.0 ± 17.2 | ≥310 | 30 249.2 ± 34.3 |
白刺 Nitraria sibirica | 78.3 ± 5.8 | 328.6 ±18.36 | ≥200 | 10 622.1 ± 26.4 |
红砂 Reaumuria soongorica | 55.0 ± 8.2 | 35.0 ± 5.6 | 80.0 ± 25.7 | 361.8 ± 19.7 |
图1 准噶尔盆地东南缘大气降水线以及植物茎水、土壤水和地下水氢、氮稳定同位素比率(δD和δ18O)值分布特征(A)、降水量的分布以及降水δ18O值季节变化特征(B)。
Fig. 1 Local meteoric water line and distribution characteristics of hydrogen and oxygen stable isotope ratio (δD and δ18O) values of stem water, soil water and groundwater (A), and precipitation distribution and the seasonal variations of δ18O value of precipitation (B) in southeast of the Junggar Desert. GMWL, global meteoric water line; LMWL, local meteoric water line.
图2 准噶尔盆地东南缘不同深度土壤含水量(A)、土壤水氧稳定同位素比率(δ18O)值(B)的变化(平均值±标准误差,n = 4)。
Fig. 2 Variations of water content (A) and oxygen stable isotope ratio (δ18O) value in soil water (B) with different soil depth in southeast of the Junggar Desert (mean ± SE, n = 4).
图3 3种荒漠植物(多枝柽柳、白刺和红砂)茎水氧稳定同位素比率(δ18O)值的变化(平均值±标准误差,n = 4)。
Fig. 3 variations of oxygen stable isotope ratio (δ18O) value of stem water of three desert plants (Tamarix ramosissima, Nitraria sibirica, Reaumuria soongorica) (mean ± SE, n = 4).
图4 3种荒漠植物(多枝柽柳、白刺和红砂)对各潜在水源的利用比例(平均值±标准误差,n = 4)。
Fig. 4 Proportion of potential water source for three desert plants (Tamarix ramosissima, Nitraria sibirica and Reaumuria soongorica) (mean ± SE, n = 4).
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