ORIGINAL RESEARCH
Soil Grain-Size Characteristics of Nitraria
tangutorum Nebkhas with Different Degrees
of Vegetation Coverage in
a Desert-Oasis Ecotone
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1
Inner Mongolia Normal University, Hohhot, China
2
Inner Mongolia Repair Engineering Laboratory of Wetland Eco-Environment System
3
Inner Mongolia Agricultural University, Hohhot, China
Submission date: 2019-09-19
Final revision date: 2019-12-17
Acceptance date: 2019-12-26
Online publication date: 2020-04-10
Publication date: 2020-06-08
Pol. J. Environ. Stud. 2020;29(5):3703-3714
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ABSTRACT
Wind erosion is an important part of environmental change research and represents a key
destabilizing factor in arid and semi-arid ecosystems. The desert-oasis ecotone is an ecological barrier
that protects oases from sandstorms. Nitraria tangutorum nebkhas help mitigate the impacts of wind
erosion in desert-oasis ecotones. This study analyzed the relationship between vegetation coverage
and soil grain size in a desert-oasis ecotone along the southeastern margin of the Tengger Desert. The
results showed that the soil grain size distributions for nebkhas consisted primarily of fine, medium
and very fine sand. The measured proportion of fine sand increased as vegetation coverage increased.
The trailing edge of leeward slope and leading edge of windward slope positions contained higher
proportions of coarse-grained material relative to other slope positions. Samples collected 0-5 cm depth
contained higher proportions of fine-grained material than those collected at 5-10 cm depth. The average
particle size ranges for nebkhas with low, medium, and high vegetation coverage were 1.644-2.430 φ,
1.601-2.911 φ, and 1.752-2.871 φ, respectively. Soil sorting degree was categorized as medium. Skewness
values were extremely negative, negative, and positive respectively, and kurtosis levels were medium,
narrow and medium, respectively. Samples collected from windward slope positions gave higher mean
grain size values than those measured from samples collected along leeward slope and the top positions.