School of Soil and Water Conservation, Beijing Forestry University, Beijing, 100083, China.
Engineering Research Center of Forestry Ecological Engineering, Ministry of Education, Beijing Forestry University, Beijing, 100083, China.
Sci Rep. 2021 Jul 23;11(1):15098. doi: 10.1038/s41598-021-94758-5.
Deep soil moisture is a highly important source of water for vegetation in the semiarid Loess Plateau of China, vegetation restoration reduced the deep soil moisture, but how to better quantify the impact of vegetation restoration on deep soil moisture is lack of certain understanding. To explore the impact exerted by different types of vegetation on deep layers of the soil moisture, the 0-10 m soil moisture content profile was measured before and after the rainy season in Armeniaca sibirica, Robinia pseudoacacia, Populus simonii, Pinus tabuliformis, Hippophae rhamnoides and in natural grassland in Wuqi County in Shannxi Province. These results showed that the highest soil moisture in the shallow layers (0-200 cm) was exhibited in the P. simonii forest, which was followed by that in the natural grassland. Both of these results were significantly higher than that those of the A. sibirica, P. tabuliformis, H. rhamnoides and R. pseudoacacia forests. The soil moisture in the deep layer (200-1000 cm) of the natural grassland was significantly higher than that of the other vegetation types. The annual precipitation that recharges the depth of soil moisture was the highest in natural grassland and the lowest in P. simonii. The inter-annual soil moisture replenishment is primarily affected by rainfall and vegetation types. Compared with the natural grassland, the CSWSD (the comparison of the soil moisture storage deficit) of different vegetation types varies. In the shallow soil layer, P. simonii is the lowest, and R. pseudoacacia is the highest. In the deep soil layer, R. pseudoacacia and P. simonii are the highest; H. rhamnoides is the second highest, and A. sibirica and P. tabuliformis are the lowest. These results indicate that vegetation restoration can significantly reduce the amount of water in the deep layers of the soil. In the future vegetation restoration, we suggest emphasizing natural development more strongly, since it can better maintain the local vegetation stability and soil moisture balance.
深层土壤水分是中国半干旱黄土高原植被的重要水源,植被恢复减少了深层土壤水分,但如何更好地量化植被恢复对深层土壤水分的影响仍缺乏一定的认识。为了探讨不同植被类型对深层土壤水分的影响,在陕西吴起县对 10 种植被类型(包括山杏、刺槐、新疆杨、油松、沙棘、柠条、天然草地)的 0-10m 土壤水分含量剖面进行了雨季前后的测量。结果表明,在浅层(0-200cm),新疆杨林的土壤水分最高,其次是天然草地。这两种结果均显著高于山杏林、油松林、沙棘林和刺槐林。天然草地的深层(200-1000cm)土壤水分显著高于其他植被类型。补给土壤水分的年降水量以天然草地最高,新疆杨最低。土壤水分的多年补给主要受降雨和植被类型的影响。与天然草地相比,不同植被类型的 CSWSD(土壤水分储存亏缺的比较)有所不同。在浅层土壤中,新疆杨最低,刺槐最高。在深层土壤中,刺槐和新疆杨最高;沙棘次之,山杏和油松最低。这些结果表明,植被恢复可以显著减少土壤深层的水分含量。在未来的植被恢复中,我们建议更加强调自然发展,因为它可以更好地保持当地植被的稳定性和土壤水分平衡。