1. 兰州城市学院 化学与环境科学学院,甘肃,兰州,730070
2. 城市环境污染控制高校省级重点实验室,甘肃,兰州,730070
3. 兰州城市学院 城市生态与环境生物技术中心,甘肃,兰州,730070
纸质出版:2014
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张鸣, 张力, 石晓妮, 等. 民勤绿洲盐生草生境土壤盐分特征及离子组成[J]. 水土保持通报, 2014,33(6):231-235.
ZHANG Ming, ZHANG Li, SHI Xiao-ni, et al. Characteristics of Soil Salinity and Ion Composition in Habitat Soil of Halogeton Glomeratus in Minqin Oasis[J]. Bulletin of Soiland Water Conservation, 2014, 33(6): 231-235.
张鸣, 张力, 石晓妮, 等. 民勤绿洲盐生草生境土壤盐分特征及离子组成[J]. 水土保持通报, 2014,33(6):231-235. DOI: 10.13961/j.cnki.stbctb.2014.06.048.
ZHANG Ming, ZHANG Li, SHI Xiao-ni, et al. Characteristics of Soil Salinity and Ion Composition in Habitat Soil of Halogeton Glomeratus in Minqin Oasis[J]. Bulletin of Soiland Water Conservation, 2014, 33(6): 231-235. DOI: 10.13961/j.cnki.stbctb.2014.06.048.
对民勤绿洲盐生草周围不同距离范围内的总体盐分状况、盐分离子组成及离子之间的相关性进行了研究。结果表明
盐生草具有一定的聚盐作用
在其周围形成了一定的"盐岛"效应。在距盐生草0-60 cm范围内
土壤剖面中的土壤盐渍化程度随土层的加深而加重
土壤阴离子主要有Cl
-
和SO
4
2-
阳离子主要有Na
+
和Ca
2+
土壤盐分主要是氯化钠、氯化钙、硫酸钠和硫酸钙
其次是氯化镁和硫酸镁。其中在盐生草周围0-40 cm范围内
垂直剖面0-20 cm土层土壤全盐含量为0.98~1.52 g/kg
属于非盐渍化土壤
20-40 cm土层土壤全盐含量达到了2.25~2.30 g/kg
属于轻度盐渍化土壤
40-60 cm土层土壤全盐含量达到了3.10~3.16 g/kg
属中度盐渍化;在距盐生草60 cm处
垂直剖面0-40 cm土层土壤全盐含量为0.83~1.86 g/kg
属非盐渍化
40-60 cm土层土壤全盐含量达到了2.43 g/kg
属轻度盐渍化。除HCO
3
-
外
土壤盐分含量与各盐分离子之间均呈极显著正相关。
Soil total salt
salt ions composition and correlations of different salt ions in habitat of Halogeton glomeratus in Minqin Oasis were studied. Results showed that H. glomeratus can accumulate salts and formed a certain salt island around its habitat. In the horizontal direction 0-60 cm away from H. glomeratus
the soil salinization degree aggravated with soil depth increases in 0-60 cm on the soil profile
among which anions were mainly Cl-
and SO42- and cations were Na+ and Ca2+. The main soil salinity were sodium chloride
calcium chloride
sodium sulfate and calcium sulfate
followed by magnesium chloride and magnesium sulfate. In 0-40 cm distance away from plant
the total salinity contents of the 0-20 cm soil layer on the soil profile were 0.98~1.52 g/kg and belonged to non-salinization soil
while that of the 20-40 cm and 40-60 cm soil layers were 2.25~2.30 g/kg and 3.10~3.16 g/kg
which belonged to light salinization soil and medium salinization soil
respectively. Furthermore
in the horizontal direction 60 cm distance away from the H. glomeratus
the total salinity content of 0-40 cm and 40-60 cm soil layers on the soil profile were 0.83~1.86 g/kg and 2.43 g/kg
which belonged to non-salinization and light salinization. There were extremely significantly positive correlations between soil salt content and ions contents except the content of HCO3-.
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LI Fahu, Keren R. Calcareous sodic soil reclamation as affected by corn stalk application and incubation:A laboratory study[J]. Pedosphere, 2009, 19(4):465-475.
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Lycium ruthenicum
)对盐渍土盐分分布的影响[J].中国沙漠,2013,33(5):1406-1412.
王海江,王开勇,刘玉国,等.膜下滴灌棉田不同土层盐分变化及其对棉花生长的影响[J].生态环境学报,2010,19(10):2381-2385.
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王海珍,韩路,贾文锁.胡杨(
Populus euphraticu
)与灰胡杨(
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