Effects of terracing with Platycladus orientalis plantations on water budget in the dryland of Loess Plateau in China

IF 4.3 3区 材料科学 Q1 ENGINEERING, ELECTRICAL & ELECTRONIC
Yue Huang , Wei Wei , Shengnan Chen , Liding Chen
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Abstract

Terracing engineering and vegetation plantation have been implemented in many water-limited areas, aiming to reduce the effect of drought, conserve water, and promote ecosystem restoration. However, due to the complexities of slope structure, the major hydrologic processes controlling the water balance of terraces are still unclear. To further quantify the role of terraces on water retention in the stand scale, in a normal year (2015) and a dry year (2016), we compared the water balance for the combination of Platycladus orientalis with zig terrace (PZ), fish scale pits (PF), and natural slope (PN) in a typical loess hilly area of China. Our results indicated that terracing was an effective way to increase water retention and reduce runoff. After the growing season, compared with PN, terraced fields enhanced the water budget with 13.6–21.3 mm for PZ and 2.4–11.7 mm for PF. In addition, terraced fields generated less runoff (a reduction of 45.3–60.8 % for PZ and 19.6–26.6 % for PF) and more soil water storage (an increase of 18.5–24.1 % for PZ and 13.6–14.7 % for PF) than the natural slope. Overall, the water budget of all plots was positive (29.6 mm for PZ > 20.0 mm for PF > 8.3 mm for PN) in the normal year (2015) and negative (−49.6 mm for PZ > −60.8 mm for PF > −63.2 mm for PN) in the dry year (2016). Our results suggest that precipitation is still the primary factor affecting the water budget in woodlands, and terracing measures can help to improve the utilization of precipitation and enhance soil water retention in the Loess Plateau.
中国黄土高原旱地梯田植树造林对水收支的影响
许多水资源有限的地区都实施了梯田工程和植被种植,旨在减少干旱影响、节约用水和促进生态系统恢复。然而,由于坡面结构复杂,控制梯田水分平衡的主要水文过程尚不清楚。为了进一步量化梯田在林分尺度上的保水作用,我们在正常年份(2015 年)和干旱年份(2016 年),比较了中国典型黄土丘陵地区东方桔梗与人字形梯田(PZ)、鱼鳞坑(PF)和自然坡(PN)组合的水平衡。我们的研究结果表明,修筑梯田是增加蓄水量和减少径流的有效方法。生长季结束后,与自然坡地相比,梯田提高了水量收支,PZ 为 13.6-21.3 毫米,PF 为 2.4-11.7 毫米。此外,与自然坡地相比,梯田产生的径流更少(PZ 减少了 45.3-60.8%,PF 减少了 19.6-26.6%),土壤蓄水量更大(PZ 增加了 18.5-24.1%,PF 增加了 13.6-14.7%)。总体而言,所有地块的水分预算在正常年份(2015 年)为正值(PZ 为 29.6 毫米;PF 为 20.0 毫米;PN 为 8.3 毫米),在干旱年份(2016 年)为负值(PZ 为-49.6 毫米;PF 为-60.8 毫米;PN 为-63.2 毫米)。我们的研究结果表明,降水仍然是影响林地水分平衡的主要因素,而梯田措施有助于提高黄土高原降水的利用率和土壤的保水性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
7.20
自引率
4.30%
发文量
567
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