荒漠草原两种类型土壤的水分动态对比

doi:10.13287/j.1001-9332.202005.012

应用生态学报 ›› 2020, Vol. 31 ›› Issue (5): 1560-1570.doi: 10.13287/j.1001-9332.202005.012

荒漠草原两种类型土壤的水分动态对比

陈晓莹, 陈林, 宋乃平^*, 李敏岚, 吴婷, 杨新国, 王磊, 王兴

宁夏大学西北退化生态系统恢复与重建教育部重点实验室/西北土地退化与生态恢复省部共建国家重点实验室培育基地, 银川 750021

收稿日期:2019-12-12 出版日期:2020-05-15 发布日期:2020-05-15
通讯作者: * E-mail: songnp@163.com
作者简介:陈晓莹, 女, 1995年生, 硕士研究生。主要从事土壤水环境研究。E-mail: 18809560650@163.com
基金资助:
宁夏回族自治区重点研发项目(2019BFG02022)、宁夏高等学校一流学科建设(生态学)项目(NXYLXK2017B06)、第三批宁夏青年科技人才托举工程项目(TJGC20180682018)和宁夏大学研究生创新项目(GIP2019046)资助

Comparison on moisture dynamics of two different soil types in desert steppe

CHEN Xiao-ying, CHEN Lin, SONG Nai-ping^*, LI Min-lan, WU Ting, YANG Xin-guo, WANG Lei, WANG Xing

Ministry of Education Key Laboratory for Restoration and Reconstruction of Degraded in Northwest China/Breeding Base for State Key Laboratory of Land Degradation and Ecological Restoration of Northwest China, Ningxia University, Yinchuan 750021, China

Received:2019-12-12 Online:2020-05-15 Published:2020-05-15
Contact: * E-mail: songnp@163.com
Supported by:
This work was supported by the Ningxia Hui Autonomous Region Key Research and Development Project (2019BFG02022), the Ningxia Higher Education First-Class Discipline Construction (Ecology) Fund (NXYLXK2017B06), the Third Batch of Ningxia Young Scientific and Technological Talent Support Project (TJGC20180682018), and the Ningxia University Graduate Innovation Project (GIP2019046).

摘要/Abstract

摘要： 基于2017—2018年的定位监测数据,分析了宁夏东部的盐池荒漠草原2种不同类型土壤(灰钙土和风沙土)的水分时空动态特征。结果表明: 2017和2018年生长季(5—10月),研究区降雨量分别为208.2和274.8 mm,降雨在各月份的分配差异较大。2018年除5月存在极端降雨事件(129.6 mm)外,其余各月降雨量均低于2017年。土壤水分变化的季节动态规律大致可以分为两个阶段:土壤水分补偿期(5月初至6月初)和土壤水分波动期(6月中旬至9月底)。0～20 cm土层土壤含水量在降雨后呈骤增骤减的脉冲式特点,深层土壤含水量较稳定。灰钙土土壤含水量随土层加深表现为“升-降-升”的变化,风沙土土壤含水量在0～60 cm土层出现井喷式增加,而后增加缓慢,但随着土层深度的增加土壤含水量逐渐增大。2017年,灰钙土全剖面(0～100 cm)土壤水分表现为积累型,风沙土表现为消耗型;2018年,两种类型的土壤水分在全剖面均表现为消耗型。两种土壤类型土壤水分的时间稳定性随土壤深度的增加而增强,灰钙土和风沙土全剖面的平均土壤含水量代表性土层分别为80～100和40～60 cm。2种类型土壤的土壤水分时空分布不同,风沙土受降水的影响高于灰钙土。降水会降低土壤水分的变异性,改变土壤水分的时间稳定性。

关键词: 荒漠草原, 土壤类型, 土壤水分, 时间稳定性

Abstract: Based on the positioning monitoring data from 2017 to 2018, we analyzed the spatial-temporal dynamic characteristics of moisture in two different soil types (sierozem and aeolian sandy soil) in the Yanchi desert steppe in the eastern Ningxia. The results showed that the rainfall in the study area was 208.2 and 274.8 mm in the growing season of 2017 and 2018 (May-October), respectively. The distribution of rainfall varied across different months. Except for the extreme rainfall event (129.6 mm) in May in 2018, rainfall in other months was lower than that in 2017. The seasonal dynamics of soil water content was roughly divided into two phases: compensation period (early May to early June) and fluctuation period (mid June to late September). The soil moisture of 0-20 cm layer had a pulse characteristic of rapid increase and decrease after rainfall, while that of the deep soil was relatively stable. The soil water content of sierozem showed a “rise-fall-liter” change with increasing soil depth. The saeolian sandy soil increased sharply from 0 to 60 cm then increased slowly, whereas soil water content gradually increased with increasing soil depth. In 2017, soil moisture in the soil profile (0-100 cm) of the sierozem was accumulated, and the aeo-lian sand soil was in the consumption type. In 2018, both soil water across the full profile in both soil types were the consumption type. The temporal stability of soil moisture of two soil types increased with increasing soil depth. The average soil water content of the whole sections of sierozem and aeolian sandy soil were 80-100 and 40-60 cm, respectively. The two soil types had different spatial and temporal distributions of soil moisture. Aeolian sandy soil was more affected by precipitation than sierozem. Precipitation would reduce the variability of soil moisture and change its temporal stability.

Key words: desert steppe, soil type, soil moisture, time stability

陈晓莹, 陈林, 宋乃平, 李敏岚, 吴婷, 杨新国, 王磊, 王兴. 荒漠草原两种类型土壤的水分动态对比[J]. 应用生态学报, 2020, 31(5): 1560-1570.

CHEN Xiao-ying, CHEN Lin, SONG Nai-ping, LI Min-lan, WU Ting, YANG Xin-guo, WANG Lei, WANG Xing. Comparison on moisture dynamics of two different soil types in desert steppe[J]. Chinese Journal of Applied Ecology, 2020, 31(5): 1560-1570.

参考文献

[1] 邵明安, 贾小旭, 王云强, 等. 黄土高原土壤干层研究进展与展望. 地球科学进展, 2016, 31(1): 14-22 [Shao M-A, Jia X-X, Wang Y-Q, et al. A review of studies on dried soil layers in the Loess Plateau. Advances in Earth Science, 2016, 31(1): 14-22]
[2] 张涵丹, 卫伟, 陈利顶, 等. 典型黄土区油松树干液流变化特征分析. 环境科学, 2015, 36(1): 349-356 [Zhang H-D, Wei W, Chen L-D, et al. Analysis of sap flow characteristics of the Chinese pine in typical Loess Plateau region of China. Environmental Science, 2015, 36(1): 349-356]
[3] 潘颜霞, 王新平. 荒漠人工植被区浅层土壤水分空间变化特征分析. 中国沙漠, 2007, 27(2): 250-256 [Pan Y-X, Wang X-P. Spatial variation of soil moisture in revegetated desert area. Journal of Desert Research, 2007, 27(2): 250-256]
[4] 刘苑秋, 王红胜, 郭圣茂, 等. 江西省退化石灰岩红壤区重建森林土壤水分与降水量和蒸发量的关系. 应用生态学报, 2008, 19(12): 2588-2592 [Liu Y-Q, Wang H-S, Guo S-M, et al. Relationships of soil moisture content with precipitation and evaporation in rehabilitated forests in degraded limestone red-soil region of Jiangxi Province. Chinese Journal of Applied Ecology, 2008, 19(12): 2588-2592]
[5] 杨磊, 卫伟, 莫保儒, 等. 半干旱黄土丘陵区不同人工植被恢复土壤水分的相对亏缺. 生态学报, 2011, 31(11): 3060-3068 [Yang L, Wei W, Mo B-R, et al. Soil water deficit under different artificial vegetation restoration in the semi-arid hilly region of the Loess Pla-teau. Acta Ecologica Sinica, 2011, 31(11): 3060-3068]
[6] Hu W, Shao MA, Han FP, et al. Watershed scale temporal stability of soil water content. Geoderma, 2010, 158: 181-198
[7] 王艳艳, 何雨江. 土壤分形结构对其水力性质的指示作用. 地学前缘, 2019, 26(6): 66-74 [Wang Y-Y, He Y-J. The indicative effect of soil fractal structure on its hydraulic properties. Earth Science Frontiers, 2019, 26(6): 66-74]
[8] 魏永霞, 王鹤, 刘慧, 等. 生物炭对黑土区土壤水分及其入渗性能的影响. 农业机械学报, 2019, 50(9): 290-299 [Wei Y-X, Wang H, Liu H, et al. Effect of biochar on soil moisture and its infiltration performance in black soil area. Transaction of the Chinese Society for Agriculture Machinery, 2019, 50(9): 290-299]
[9] 邵明安, 王全九, Horton R. 推求土壤水分运动参数的简单入渗法. Ⅰ. 理论分析. 土壤学报, 2000, 37(1): 1-8 [Shao M-A, Wang Q-J, Horton R. A simple infiltration method for estimating soil hydraulic properties of unsaturated soils. Ⅰ. Theoretical analysis. Acta Pedo-logica Sinica, 2000, 37(1): 1-8]
[10] Villarreal R, Lozano LA, Melani EM, et al. Diffusivity and sorptivity determination at different soil water contents from horizontal infiltration. Geoderma, 2019, 338: 88-96
[11] Solekhudin I. Time-dependent infiltration from periodic semi-circular channels with two different types of root-water uptake. Proceedings of the 1st Annual International Conference on Mathematics, Science, and Education (ICoMSE 2017), Malang, Indonesia, 2017: 26-30
[12] Vachaud G, Silans APD, Balabanis P, et al. Temporal stability of spatially measured soil water probability density function. Soil Science Society of America Journal, 1985, 49: 822-828
[13] Hawley ME, Jackson TJ, McCuen RH. Surface soil moisture variation on small agricultural watersheds. Journal of Hydrology, 1983, 62: 179-200
[14] da Silva AP, Nadler A, Kay BD. Factors contributing to temporal stability in spatial patterns of water content in the tillage zone. Soil and Tillage Research, 2001, 58: 207-218
[15] Mohanty BP, Skaggs TH. Spatio-temporal evolution and time-stable characteristics of soil moisture within remote sensing footprints with varying soil, slope, and vegetation. Advances in Water Resources, 2001, 24: 1051-1067
[16] Jacobs JM, Mohanty BP, Hsu EC, et al. SMEX02: Field scale variability, time stability and similarity of soil moisture. Remote Sensing of Environment, 2004, 92: 436-446
[17] 赵亚楠, 于露, 周玉蓉, 等. 宁夏东部荒漠草原灌丛引入对土壤水分动态及亏缺的影响. 生态学报, 2020, 40(4): 1305-1315 [Zhao Y-N, Yu L, Zhou Y-R, et al. Soil moisture dynamics and deficit of desert grassland with anthropogenic introduced shrub encroachment in the eastern Ningxia, China. Acta Ecologica Sinica, 2020, 40(4): 1305-1315]
[18] 曲潇琳, 龙怀玉, 谢平, 等. 宁夏中部地区典型灰钙土的发育特性及系统分类研究. 土壤学报, 2018, 55(1): 75-87 [Qu X-L, Long H-Y, Xie P, et al. Gene-tic characteristics and classification of typical sierozem in central Ningxia, China. Acta Pedologica Sinica, 2018, 55(1): 75-87]
[19] 沈海花, 朱言坤, 赵霞, 等. 中国草地资源的现状分析. 科学通报, 2016, 61(2): 139-154 [Shen H-H, Zhu Y-K, Zhao X, et al. Analysis of current grassland resources in China. Chinese Science Bulletin, 2016, 61(2): 139-154]
[20] 韩晓阳, 刘文兆, 程立平. 黄土塬区深剖面土壤水分垂直分布特征及其时间稳定性. 应用生态学报, 2017, 28(2): 430-438 [Han X-Y, Liu W-Z, Cheng L-P. Vertical distribution characteristics and temporal stability of soil water in deep profile on the Loess Tableland, Northwest China. Chinese Journal of Applied Eco-logy, 2017, 28(2): 430-438]
[21] 陈洪松, 邵明安, 王克林. 黄土区荒草地和裸地土壤水分的循环特征. 应用生态学报, 2005, 16(10): 1853-1857 [Chen H-S, Shao M-A, Wang K-L. Water cycling characteristics of grassland and bare land soils on Loess Plateau. Chinese Journal of Applied Ecology, 2005, 16(10): 1853-1857]
[22] 杨启红, 陈丽华, 张富, 等. 土壤水分变异对降雨和植被的响应. 北京林业大学学报, 2008, 30(suppl.2): 88-94 [Yang Q-H, Chen L-H, Zhang F, et al. Responses of soil moisture variations to rainfall and vegetation. Journal of Beijing Forestry University, 2008, 30(suppl.2): 88-94]
[23] 冯金超, 党宏忠, 丛日春, 等. 黄土区不同土地利用方式下土壤水分动态特征. 山东农业大学学报:自然科学版, 2019, 50(4): 729-734 [Feng J-C, Dang H-Z, Cong R-C, et al. Dynamic characteristics of soil moisture under different land use type in loess region. Journal of Shandong Agricultural University: Natural Science, 2019, 50(4): 729-734]
[24] 张敏, 刘爽, 刘勇, 等. 黄土丘陵缓坡风沙区不同土地利用类型土壤水分变化特征. 水土保持学报, 2019, 33(3): 115-120 [Zhang M, Liu S, Liu Y, et al. Soil moisture variation characteristics of different land use types in the moderate slope sandy area of loess hilly region. Journal of Soil and Water Conservation, 2019, 33(3): 115-120]
[25] 秦海琴, 展秀丽, 张萍. 宁夏白芨滩固定沙丘浅层土壤水分时空变异. 云南农业大学学报:自然科学版, 2020, 35(1): 160-167 [Qin H-Q, Zhan X-L, Zhang P. Temporal and spatial variation of soil moisture in the shallow dune fixed on Baijitan in Ningxia. Journal of Yunnan Agricultural University: Natural Science, 2020, 35(1): 160-167]
[26] 周宏飞, 肖祖炎, 姚海娇, 等. 古尔班通古特沙漠树枝状沙丘土壤水分时空变异特征. 水科学进展, 2013, 24(6): 771-777 [Zhou H-F, Xiao Z-Y, Yao H-J, et al. Temporal and spatial variation of soil moisture in dendritic sand dune over Gurbantunggut desert in central Eurasia. Advances in Water Science, 2013, 24(6): 771-777]
[27] 朱海, 胡顺军, 陈永宝. 古尔班通古特沙漠南缘固定沙丘土壤水分时空变化特征. 土壤学报, 2016, 53(1): 117-126 [Zhu H, Hu S-J, Chen Y-B. Temporal and spatial variations of soil moisture in fixed dunes in the southern edge of the Gurbantungut desert. Acta Pedologica Sinica, 2016, 53(1): 117-126]
[28] 叶冬梅, 秦佳琪, 韩胜利, 等. 乌兰布和沙漠流动沙地土壤水分动态、土壤水势特征的研究. 干旱区资源与环境, 2005, 19(3): 126-130 [Ye D-M, Qin J-Q, Han S-L, et al. Study on soil water dynamics and soil water potential characteristics of flowing sandy land in Ulanbuhe desert. Journal of Arid Land Resources and Environment, 2005, 19(3): 126-130]
[29] 徐志尧, 张钦弟, 杨磊. 半干旱黄土丘陵区土壤水分生长季动态分析. 干旱区资源与环境, 2018, 32(3): 145-151 [Xu Z-Y, Zhang Q-D, Yang L. Analysis of temporal variation of soil water in a growing season in semi-arid loess hilly area. Journal of Arid Land Resources and Environment, 2018, 32(3): 145-151]
[30] 樊军, 郝明德, 邵明安. 黄土旱塬农业生态系统土壤深层水分消耗与水分生态环境效应. 农业工程学报, 2004, 20(1): 61-64 [Fan J, Hao M-D, Shao M-A. Water consumption of deep soil layers and eco-environmental effects of agricultural ecosystem in the Loess Plateau. Transactions of the Chinese Society of Agricultural Engineering, 2004, 20(1): 61-64]
[31] 王艳莉, 刘立超, 高艳红, 等. 人工固沙植被区土壤水分动态及空间分布. 中国沙漠, 2015, 35(4): 942-950 [Wang Y-L, Liu L-C, Gao Y-H, et al. Dynamic and spatial distribution of soil moisture in an artificially re-vegetated desert area. Journal of Desert Research, 2015, 35(4): 942-950]
[32] 乔江波, 朱元骏, 贾小旭, 等. 黄土高原关键带全剖面土壤水分空间变异性. 水科学进展, 2017, 28(4): 515-522 [Qiao J-B, Zhu Y-J, Jia X-X, et al. Spatial variability of soil water for the entire profile in the critical zone of the Loess Plateau. Advances in Water Science, 2017, 28(4): 515-522]
[33] 胡双熙, 张维祥, 张建明, 等. 青甘宁地区灰钙土的成土特点. 兰州大学学报:自然科学版, 1990, 26(3): 127-136 [Hu S-X, Zhang W-X, Zhang J-M, et al. Characteristics of grey calcareous soil in Qingganning region. Journal of Lanzhou University: Natural Science, 1990, 26(3): 127-136]
[34] 赵丹, 李惠, 苏彦苹, 等. 不同立地、土壤类型对土壤含水量和苹果新梢生长的影响. 河北林果研究, 2016, 31(1): 25-32 [Zhao D, Li H, Su Y-P, et al. Effects of different sites and soil types on soil water content and apple shoot growth. Hebei Journal of Forestry and Orchard Research, 2016, 31(1): 25-32]
[35] 兰志龙, 潘小莲, 赵英, 等. 黄土丘陵区不同土地利用模式对深层土壤含水量的影响. 应用生态学报, 2017, 28(3): 847-855 [Lan Z-L, Pan X-L, Zhao Y, et al. Effects of land use types on deep soil water content in the loess hilly area of the north Shaanxi Province, China. Chinese Journal of Applied Ecology, 2017, 28(3): 847-855]
[36] Gao XD, Wu PT, Zhao XI, et al. Soil moisture variabi-lity along transects over a well-developed gully in the Loess Plateau, China. Catena, 2011, 87: 357-367
[37] Jawson SD, Niemann JD. Spatial patterns from EOF analysis of soil moisture at a large scale and their dependence on soil, land-use, and topographic properties. Advances in Water Resources, 2006, 30, DOI: 10.1016/j.advwatres.2006.05.006
[38] 吴江琪, 马维伟, 李广, 等. 黄土高原4种植被类型对土壤物理特征及渗透性的影响. 水土保持学报, 2018, 32(4): 133-138 [Wu J-Q, Ma W-W, Li G, et al. Effects of 4 types of plant cover on soil physical cha-racteristics and permeability in the Loess Plateau. Journal of Soil and Water Conservation, 2018, 32(4): 133-138]
[39] 陈洪松, 邵明安. 黄土区坡地土壤水分运动与转化机理研究进展. 水科学进展, 2003, 14(4): 413-420 [Chen H-S, Shao M-A. Review on hills-lope soil water movement and transformation mechanism on the Loess Plateau. Advances in Water Science, 2003, 14(4): 413-420]
[40] Yang WZ, Shao MA, Peng XD, et al. On the relationship between environmental aridization of the Loess Pla-teau and soil water in loess. Science in China Series D:Earth Sciences, 1999, 42: 240-249
[41] 高思远, 张建军, 李梁, 等. 黄土区水土保持林地的蓄水动态及雨水渗透深度. 中国水土保持科学, 2019, 17(2): 17-26 [Gao S-Y, Zhang J-J, Li L, et al. Water storage dynamics and rainwater penetration depth of soil and water conservation forest land in the Loess Plateau. Science of Soil and Water Conservation, 2019, 17(2): 17-26]
[42] 尹笑笑, 王东. 两种土壤质地麦田贮水量与表层土壤水分的关系. 麦类作物学报, 2018, 38(7): 841-853[Yin X-X, Wang D. Relationship between water storage in wheat field and surface soil moisture in two soil texture. Journal of Triticeae Crops, 2018, 38(7): 841-853]
[43] 赵磊磊, 朱清科, 聂立水, 等. 陕北黄土区陡坡土壤水分变异规律研究. 生态环境学报, 2012, 21(2): 253-259 [Zhao L-L, Zhu Q-K, Nie L-S, et al. Variation of soil moisture on steep slope in loess region of Northern Shanxi. Ecology and Environment, 2012, 21(2): 253-259]
[44] 蒋太明, 刘海隆, 刘洪斌, 等. 黄壤坡地土壤水分垂直变异特征分析. 农业工程学报, 2005, 21(3): 6-11 [Jiang T-M, Liu H-L, Liu H-B, et al. Analysis of vertical variability of soil moisture on sloping land in yellow soil. Transactions of the Chinese Society of Agricultural Engineering, 2005, 21(3): 6-11]
[45] 潘成忠, 上官周平. 黄土半干旱丘陵区陡坡地土壤水分空间变异性研究. 农业工程学报, 2003, 19(6): 5-9 [Pan C-Z, Shangguan Z-P. Spatial variability of soil moisture on steep slope land in loess hill region. Transactions of the Chinese Society of Agricultural Engineering, 2003, 19(6): 5-9]
[46] 王晓军, 武江涛, 王兵, 等. 黄土丘陵沟壑区小流域土壤水分空间变异. 生态学杂志, 2015, 34(9): 2568-2575 [Wang X-J, Wu J-T, Wang B, et al. Spatial variability of soil moisture in hilly and gully Loess Plateau. Chinese Journal of Ecology, 2015, 34(9): 2568-2575]
[47] 贾小旭, 邵明安, 张晨成, 等. 黄土高原南北样带不同土层土壤水分变异与模拟. 水科学进展, 2016, 27(4): 520-528 [Jia X-X, Shao M-A, Zhang C-C, et al. Variation and simulation of soil water content within different soil depths along the south-north transect of the Loess Plateau. Advances in Water Science, 2016, 27(4): 520-528]
[48] 白一茹, 王幼奇, 王建宇. 黄土丘陵区枣林土壤水分时间稳定性特征. 应用基础与工程科学学报, 2018, 26(1): 23-34 [Bai Y-R, Wang Y-Q, Wang J-Y. Temporal stability of soil moisture on jujube orchard in loess hilly region. Journal of Basic Science and Engineering, 2018, 26(1): 23-34]
[49] Jia YH, Shao MA. Temporal stability of soil water sto-rage under four types of revegetation on the northern Loess Plateau of China. Agricultural Water Management, 2013, 117: 33-42
[50] Qiu Y, Fu BJ, Wang J, et al. Spatial variability of soil moisture content and its relation to environmental indices in a semi-arid gully catchment of the Loess Plateau of China. Journal of Arid Environments, 2001, 49: 723-750
[51] Hu W, Shao MA, Han FP, et al. Watershed scale temporal stability of soil water content. Geoderma, 2010, 158: 181-198
[52] Famiglietti JS, Rudnicki JW, Rodell M. Variability in surface moisture content along a hillslope transect: Rattlesnake hill. Journal of Hydrology, 1998, 210: 259-281
[53] 信秀丽, 张佳宝, 朱安宁. 土壤水吸力空间分布规律的时间稳定性研究. 农业工程学报, 2008, 24(5): 15-19 [Xin X-L, Zhang J-B, Zhu A-N. Temporal stability of spatial distribution pattern of soil water tension at different scales. Transactions of the Chinese Society of Agricultural Engineering, 2008, 24(5): 15-19]

荒漠草原两种类型土壤的水分动态对比

Comparison on moisture dynamics of two different soil types in desert steppe

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