[1]Hamit·Yimit,Anwar·Eziz,Saydigul·Haxim,et al.Spatial Variation of Soil Water Content in Keriya Oasis in Xinjiang[J].Research of Soil and Water Conservation,2013,20(02):127-134.
Copy
Spatial Variation of Soil Water Content in Keriya Oasis in Xinjiang
Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume:
20
Number of periods:
2013 02
Page number:
127-134
Column:
Public date:
2013-04-28
- Title:
- Spatial Variation of Soil Water Content in Keriya Oasis in Xinjiang
- Keywords:
- Keriya oasis; soil water content; spatial variability
- CLC:
- S152.7
- DOI:
- -
- Abstract:
- A zonal reeds land located in western part of Karki Village in Keriya Oasis was chosed as a study area, 28 sample points were arranged, the reeds, growth indices such as coverage, height, crown length, crown width and density were collected, three soil layers 0—10, 10—30, 30—50 cm was apareed to take the soil samples. On the bases of soil moisture data, the spatial variability of soil characteristics of reeds land was studied by using the descriptive statistical analysis and geostatistical analysis. And then, the relationship between soil water content in each layer and the growth of reeds was analyzed by using the correlation analysis in order to provide a theoretical base for improving the weak ecosystem of the study area. It could be infered that soil moisture on three layers exhibited medium spatial variability based on the descriptive statistical analysis. Soil moisture increased with the increase of soil depth, but the degree of decreased. Characteristics of vertical distribution of soil water content had four distribution types including the bottom assembled type, medio-assembled type, surface assembled type and combination of bottom and surface assembled type. Bottom assembled type was the major soil moisture profile type in this area, followed by the medio-assembled type, then combination of bottom and surface assembled type, the distribution area of surface assembled soil water content profile was the minimum. Correlation analysis between growth of reeds and soil moisture showed that the amount of soil water of each layer and reed growth was positively correlated. The positive effect of soil water content on the growth of reed cover, plant height and density was less obvious compared to its effect on reed crown length and crown width. Soil water content in deep layer played more important role than soil water content of upper layer in promoting the reed growth.
- References:
-
[1] 丁建丽,塔西甫拉提·特依拜,熊黑钢,等.塔里木盆地南缘绿洲荒漠化动态变化遥感研究:以策勒县为例[J].遥感学报,2002,6(1):56-62.
[2] Comegna V, Vitale C. Space-time analysis of water status in a Volcanic Vesuvian soil[J]. Geoderma,1993,60(1/4):135-158.
[3] Reichard K, Bacchi O S S. Hydraulic variability in space and time in a dark red latosol of the tropics[J]. Geoderma,1993,60(4):159-168.
[4] 李鸿杰,杜历.土壤水、盐入渗变异特性及其相互关系的空间序列分析[J].土壤学报,1993,30(1):60-68.
[5] 李保国,龚元石,左强,等.农田土壤水的动态模型及其应用[M].北京:科学出版,2000.
[6] 王志强,刘宝元,王晓兰.黄土高原半干旱区天然锦鸡儿灌丛对土壤水分的影响[J].地理研究,2005,24(1):113-120.
[7] 熊黑钢,徐长春.克里雅绿洲土地景观格局动态变化与预测[J].干旱区资源与环境,2008,22(6):56-62.
[8] 张爽,郭成久,苏芳莉,等.不同盐度水灌溉对芦苇生长的影响[J].沈阳农业大学学报,2008,39(1):65-68.
[9] 杨帆,邓伟,章光新.苏打盐渍土地区芦苇地土壤盐分离子空间变异与群落关系研究[J].土壤学报,2008,45(4):594-600.
[10] 李刚,苏芳莉,王铁良,等.磷溶液灌溉对芦苇生长的影响[J].中国农村水利水电,2009(7):28-30.
[11] 何玉惠,赵哈林,刘新平,等.科尔沁沙地典型生境下芦苇的生长特征分析[J].中国沙漠,2009,29(2):288-292.
[12] 唐卫东,李萍萍,卢章平.湿地芦苇发育模拟模型的研究[J].农业现代化研究,2007,28(4):510-512.
[13] 郭欢.芦苇中活性物质对有毒藻类抑制作用的研究[J].现代农业科技,2009(9):234-235.
[14] 关法春,闫超,梁正伟.盐碱化湿地芦苇群落围封和过牧条件下土壤和植被变化[J].湿地科学,2009,7(1):47-52.
[15] 贺凌云.克里雅县平原绿洲及其绿洲—荒漠交错带景观局变化分析[D].乌鲁木齐:新疆大学,2005.
[16] 塔西甫拉提·特依拜,赵睿一,丁建丽,等.干旱区绿洲LUCC马尔柯夫过程分析:以新疆克里雅绿洲为例[J].干旱区地理,2006,29(4):548-556.
[17] 刘国华.克里雅绿洲土壤盐分特征及其成盐驱动因子分析[D].乌鲁木齐:新疆大学,2005.
[18] 徐建华.现代地理学中的数学方法[M].北京:高等教育出版社,2006.
[19] 汤国安.ArcGIS地理信息系统空间分析实验教程[M].北京:科学出版社,2006.
- Similar References:
Memo
-
Last Update:
1900-01-01