Effects of alpine meadow degradation on the soil physical and chemical properties in Maqu, China

IF 2.3 4区 地球科学 Q4 GEOGRAPHY, PHYSICAL
KeCun Zhang , JiaPeng Pan , ZhiShan An , Yu Zhang , YanPing Yu
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Abstract

While alpine meadow degradation presents a significant ecological challenge, research on the complex patterns of soil property changes induced by degradation has been somewhat limited. In this study, we investigated the Maqu alpine meadow, meticulously categorizing it into different grassland types exhibiting varying degrees of degradation based on factors such as vegetation coverage and community, soil characteristics, and landscape features. These classifications included typical grassland, degraded grassland, desertified grassland, and sandy land. In August 2018, we established three quadrats at each sample point and collected soil samples at five depths (surface (0–2 cm), 2–5 cm, 5–10 cm, 10–20 cm, and 20–40 cm) to analyze soil particle size distribution (PSD) and nutrients content. The results revealed a discernible trend: alpine meadow degradation led to selective loss of nutrient-rich soil fine particles, resulting in significant alterations in soil PSD and nutrients, particularly pronounced in grasslands with low degrees of degradation. Moreover, within a specific range of degradation degree, the clay content in the shallow soil of alpine meadow increased with the degradation degree, but it declined when the degradation degree exceeded a certain threshold. Degradation also disrupted the intricate relationship between soil nutrients, with notable variations in their coupling. This difference was also reflected in the influence of soil physical and chemical properties on soil nutrients, with the explanatory power of each environmental indicator on soil nutrients decreasing significantly with increasing degradation. This study systematically analyzed the variation in soil physical and chemical properties throughout the degradation process, revealing the mechanism of soil nutrient imbalance and decline caused by the degradation process. It provides crucial theoretical foundations and reference points for the preservation and rejuvenation of alpine meadows, enriching the methodology for assessing the impact of grassland degradation.
玛曲高寒草甸退化对土壤理化性质的影响
虽然高寒草甸退化是一个重大的生态挑战,但对退化引起的土壤性质变化的复杂模式的研究有限。本研究以玛曲高寒草甸为研究对象,根据植被覆盖度、群落特征、土壤特征、景观特征等因素,将玛曲高寒草甸划分为退化程度不同的草地类型。这些分类包括典型草地、退化草地、沙化草地和沙地。2018年8月,我们在每个样点建立3个样方,在5个深度(表层(0-2 cm)、2-5 cm、5-10 cm、10-20 cm和20-40 cm)采集土壤样品,分析土壤粒径分布(PSD)和养分含量。结果表明:高寒草甸退化导致富营养土壤细颗粒的选择性损失,导致土壤PSD和养分发生显著变化,特别是在退化程度较低的草地上。在特定的退化程度范围内,高寒草甸浅层土壤粘土含量随退化程度的增加而增加,但当退化程度超过一定阈值时,粘土含量下降。退化还破坏了土壤养分之间错综复杂的关系,它们之间的耦合发生了显著变化。这种差异还体现在土壤理化性质对土壤养分的影响上,各环境指标对土壤养分的解释力随退化程度的增加而显著降低。本研究系统分析了整个退化过程中土壤理化性质的变化,揭示了退化过程导致土壤养分失衡和退化的机理。这为高寒草甸的保护和恢复提供了重要的理论基础和参考点,丰富了草地退化影响评估的方法。
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1.40
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