Groundwater table prediction and seasonal variation influenced by short rotation willow plantation on marginal riparian lands of the Prairie potholes in Canada

IF 3.1 2区 农林科学 Q2 SOIL SCIENCE
Shayeb Shahariar , Raju Soolanayakanahally , Angela Bedard-Haughn
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Abstract

Shallow groundwater consumption via phreatophytic transpiration and resulting vegetation-linked groundwater table (GWT) fluctuation is a typical soil hydrological process in wetland riparian areas. However, upland and riparian land use alterations may further influence the shallow GWT fluctuation, temporally and spatially. In this multi-year field study, we investigated whether introducing short rotation willow (SRW) positively or negatively affects the shallow GWT, soil water availability, and soil health on marginal riparian lands of the Prairie Pothole Region (PPR). We compared the impact of SRW on these parameters to two common land uses: annual crop (AC) and pasture (PA). Depth to GWT was monitored via data loggers from 28 wells in two semi-arid PPR sites. The GWT depth varied by land use practices only in site B (p < 0.001; PA > SRW = AC) but not significantly in site A (p = 0.325), and the patterns were inconsistent between sites. In GWT depth prediction, the performance of Artificial Neural Network (ANN) was better than Autoregressive Integrated Moving Average (ARIMA) models but was inconsistent alike with field observations. The GWT depth responded to seasonal precipitation and potential evapotranspiration (ET) patterns. The monthly GWT fluctuations peaked between June and August due to increased precipitation, while they were lower during May and September with reduced precipitation; however, these variations were not significant (p > 0.05). Higher precipitation and lower potential ET throughout the wet year (i.e., in 2014) significantly (p < 0.05) raised GWT (i.e., decreased depth to GWT) under all land uses, and vice versa. Our study indicated that planting SRW in marginal riparian land of the PPR would not negatively impact shallow GWT or soil water availability. Moreover, the SRW plantation could also help manage soil salinity without severely depleting the soil's nutrient pools or diminishing soil quality and health indicator parameters measured during the first rotation.

加拿大草原洼地边缘河岸土地上短轮伐柳树种植对地下水位预测和季节变化的影响
通过植被蒸腾作用消耗浅层地下水并导致与植被相关的地下水位(GWT)波动是湿地河岸地区典型的土壤水文过程。然而,高地和河岸土地利用的改变可能会在时间和空间上进一步影响浅层地下水位的波动。在这项为期多年的实地研究中,我们调查了在草原洼地地区(PPR)的边缘河岸土地上引入短轮柳(SRW)是否会对浅层 GWT、土壤水分可用性和土壤健康产生积极或消极影响。我们将 SRW 对这些参数的影响与两种常见的土地利用方式进行了比较:一年生作物(AC)和牧草(PA)。在两个半干旱的 PPR 地点,通过 28 口水井的数据记录器对 GWT 深度进行了监测。GWT 深度仅在 B 站点因土地利用方式而异(p < 0.001; PA > SRW = AC),但在 A 站点并不显著(p = 0.325),而且不同站点之间的模式也不一致。在 GWT 深度预测方面,人工神经网络(ANN)的性能优于自回归综合移动平均(ARIMA)模型,但与实地观测结果不一致。GWT 深度对季节性降水和潜在蒸散(ET)模式做出了反应。由于降水量增加,每月 GWT 波动在 6 月至 8 月期间达到峰值,而在 5 月至 9 月期间,由于降水量减少,GWT 波动较小;然而,这些变化并不显著(p > 0.05)。在整个湿润年份(即 2014 年),较高的降水量和较低的潜在蒸散发在所有土地利用条件下都显著提高了 GWT(即降低了 GWT 深度)(p < 0.05),反之亦然。我们的研究表明,在泛珠江三角洲的边缘河岸土地上种植 SRW 不会对浅层 GWT 或土壤水分可用性产生负面影响。此外,SRW 种植还有助于管理土壤盐碱化,而不会严重消耗土壤的养分库,也不会降低第一个轮作期测量的土壤质量和健康指标参数。
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来源期刊
Geoderma Regional
Geoderma Regional Agricultural and Biological Sciences-Soil Science
CiteScore
6.10
自引率
7.30%
发文量
122
审稿时长
76 days
期刊介绍: Global issues require studies and solutions on national and regional levels. Geoderma Regional focuses on studies that increase understanding and advance our scientific knowledge of soils in all regions of the world. The journal embraces every aspect of soil science and welcomes reviews of regional progress.
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