干旱区研究 ›› 2025, Vol. 42 ›› Issue (8): 1426-1436.doi: 10.13866/j.azr.2025.08.07 cstr: 32277.14.AZR.20250807
袁子喧1,3(
), 辛智鸣1,2,3, 程一本1(
), 于涛1, 刘昱萱1
收稿日期:2025-01-17
修回日期:2025-06-10
出版日期:2025-08-15
发布日期:2025-11-24
通讯作者:
程一本. E-mail: chengyiben@bjfu.edu.cn作者简介:袁子喧(2003-),女,硕士研究生,主要从事退化生态系统修复与管理研究. E-mail: Yzx0124@bjfu.edu.cn
基金资助:
YUAN Zixuan1,3(
), XIN Zhiming1,2,3, CHENG Yiben1(
), YU Tao1, LIU Yuxuan1
Received:2025-01-17
Revised:2025-06-10
Published:2025-08-15
Online:2025-11-24
摘要: 为明确乌兰布和沙漠地区有限水资源条件下多枝柽柳(Tamarix ramosissima)的蒸腾耗水动态特征及其与环境因子的关系,本研究利用包裹式液流仪对乌兰布和沙漠地区人工种植的多枝柽柳树干液流量进行监测,同时对气象和土壤水分等环境因子同步进行监测。结果表明:(1) 生长季内,多枝柽柳的树干液流量呈现先升高后降低的趋势,累计树干液流量为50.96 kg,日平均树干液流量为380.27 g,且具有明显的季节性变化特征。(2) 不同天气条件下,多枝柽柳的树干液流量日变化情况存在明显差异。晴天时的树干液流量大于阴天时的树干液流量,雨天时多枝柽柳的树干液流速率在降雨时段明显下降。连续典型晴天时,多枝柽柳存在明显的夜间蒸腾现象,白天的树干液流量为夜间树干液流量的8.6倍左右。(3) 整体来看,多枝柽柳的树干液流量与地下100 cm深处的土壤含水量、饱和水汽压差和光合有效辐射存在统计显著的强正相关关系,但相关系数提示实际关联强度可能较低,这可能是柽柳对当地干旱环境已较为适应,表现出较强的生态适应性。研究结果可为干旱沙区生态水资源补给的高效利用和固沙植被的梯度配置及生态可持续管理提供数据支持。
袁子喧, 辛智鸣, 程一本, 于涛, 刘昱萱. 乌兰布和沙漠地区多枝柽柳蒸腾耗水特征及其与环境因子的关系[J]. 干旱区研究, 2025, 42(8): 1426-1436.
YUAN Zixuan, XIN Zhiming, CHENG Yiben, YU Tao, LIU Yuxuan. Transpiration and water consumption characteristics of Tamarix ramosissima in the Ulan Buh Desert and their relationship with environmental factors[J]. Arid Zone Research, 2025, 42(8): 1426-1436.
表2
多枝柽柳的树干液流与环境因子的相关性分析"
| 环境因子 | 5月 | 6月 | 7月 | 8月 | 9月 | 5—9月 |
|---|---|---|---|---|---|---|
| 平均气温/℃ | 0.413 | 0.433* | -0.116 | -0.442* | -0.255 | 0.051 |
| 最高气温/℃ | 0.431* | 0.537** | -0.020 | -0.369* | 0.081 | 0.138 |
| 最低气温/℃ | 0.290 | 0.298 | -0.248 | -0.415* | -0.271 | -0.043 |
| 相对湿度/% | 0.291 | -0.080 | -0.378* | 0.018 | 0.209 | -0.081 |
| 饱和水汽压差/kPa | -0.146 | -0.488** | 0.214 | -0.035 | -0.357 | 0.241** |
| 光合有效辐射/(μmol·m-2·s-1) | 0.423* | 0.120 | 0.295 | -0.128 | 0.114 | 0.266** |
| 降雨量/mm | -0.026 | -0.168 | -0.191 | -0.052 | 0.481* | -0.007 |
| 10 cm土壤含水量/(m3·m-3) | -0.345 | -0.098 | 0.160 | -0.373* | -0.150 | -0.082 |
| 50 cm土壤含水量/(m3·m-3) | 0.147 | -0.218 | 0.445* | -0.339 | -0.384 | 0.061 |
| 100 cm土壤含水量/(m3·m-3) | 0.124 | -0.146 | 0.690** | -0.332 | -0.294 | 0.185* |
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