Abstract
Abstract. Hydrologic viability, in terms of moisture availability, is fundamental to ecosystem sustainability in arid and semi-arid regions. In this study, we examine the spatial distribution and after-planting variations of soil moisture content (SMC) in black locust tree (Robinia pseudoacacia L.) plantings in the Loess Plateau of China at a regional scale. Thirty sites (5 to 45 yr old) were selected, spanning an area of 300 km by 190 km in the northern region of the Shaanxi Province. The SMC was measured to a depth of 100 cm at intervals of 10 cm. Geographical, topographic and vegetation information was recorded, and soil organic matter was evaluated. The results show that, at the regional scale, SMC spatial variability was most highly correlated with rainfall. The negative relationship between the SMC at a depth of 20–50 cm and the stand age was stronger than at other depths, although this relationship was not significant at a 5 % level. Watershed analysis shows that the after-planting SMC variation differed depending upon precipitation. The SMC of plantings in areas receiving sufficient precipitation (e.g., mean annual precipitation (MAP) of 617 mm) may increase with stand age due to improvements in soil water-holding capacity and water-retention abilities after planting. For areas experiencing water shortages (e.g., MAP = 509 mm), evapotranspiration may cause planting soils to dry within the first 20 yr of growth. It is expected that, as arid and semi-arid plantings age, evapotranspiration will decrease, and the soil profile may gradually recover. In extremely dry areas (e.g., MAP = 352 mm), the variation in after-planting SMC with stand age was found to be negligible. The MAP can be used as an index to divide the study area into different ecological regions. Afforestation may sequentially exert positive, negative and negligible effects on SMCs with a decrease in the MAP. Therefore, future restoration measures should correspond to the local climate conditions, and the MAP should be a major consideration for the Loess Plateau. Large-scale and long-term research on the effects of restoration projects on SMCs is needed to support more effective restoration policies. The interaction between afforestation and local environmental conditions, particularly water availability to plants, should be taken into account in afforestation campaigns in arid and semi-arid areas.
Highlights
IntroductionAfforestation and reforestation (artificial forestation) have been implemented extensively (Del Lungo et al, 2006), and increasing attention has been paid to their ecological impact
Over the past century, afforestation and reforestation have been implemented extensively (Del Lungo et al, 2006), and increasing attention has been paid to their ecological impact
Due to the deep groundwater levels, precipitation is the only source of soil moisture, which strengthens the relationship between the soil moisture content (SMC) and mean annual precipitation (MAP)
Summary
Afforestation and reforestation (artificial forestation) have been implemented extensively (Del Lungo et al, 2006), and increasing attention has been paid to their ecological impact. Artificial forestation was initially undertaken as an effective way to alleviate water loss and soil erosion, control desertification and conserve biodiversity (Lugo, 1997; Parrotta et al, 1997; Chirino et al, 2006; Barlow et al, 2007; Porto et al, 2009). It has recently gained attention as a potential mechanism for carbon sequestration (Wright et al, 2000; Fang et al, 2001; Pacala and Socolow, 2004; Marin-Spiotta et al, 2009).
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