1. 西北农林科技大学 水利与建筑工程学院, 旱区节水农业研究院, 陕西 杨凌,712100
2. 西北农林科技大学 水土保持研究所, 黄土高原土壤侵蚀与旱地农业国家重点实验室, 陕西 杨凌,712100
纸质出版:2023
移动端阅览
袁心皓, 王馨瑶, 李凡, 等. 渐次解冻土壤粒级沉降分选及碳氮盐分布特征[J]. 水土保持通报, 2023,43(5):35-44.
Yuan Xinhao, Wang Xinyao, Li Fan, et al. Soil Particle Settlement Sorting and Distribution Characteristics of Carbon, Nitrogen and Salt During Gradual Thawing[J]. Bulletin of Soiland Water Conservation, 2023, 43(5): 35-44.
袁心皓, 王馨瑶, 李凡, 等. 渐次解冻土壤粒级沉降分选及碳氮盐分布特征[J]. 水土保持通报, 2023,43(5):35-44. DOI: 10.13961/j.cnki.stbctb.2023.05.005.
Yuan Xinhao, Wang Xinyao, Li Fan, et al. Soil Particle Settlement Sorting and Distribution Characteristics of Carbon, Nitrogen and Salt During Gradual Thawing[J]. Bulletin of Soiland Water Conservation, 2023, 43(5): 35-44. DOI: 10.13961/j.cnki.stbctb.2023.05.005.
[目的
]
将解冻逐层剥离过程与粒级沉降模拟相结合,探究融雪径流情景下坡面土壤逐层解冻过程中泥沙粒级分选规律及伴随的碳氮盐分布特性,为深入揭示东北坡面土层冻融侵蚀机理及伴生的微环境效应提供依据。[方法
]
以东北坡面黑土为例,开展了土柱冻融试验,主要包括非冻融、全冻全融与冻结后渐次解冻(土柱置于浸水环境,由外至内分融化出T
1
—T
3
3层)处理,借助沉降管对各处理的土壤进行粒级沉降分选试验,对各分选粒级电导率(EC)、pH值、有机碳(SOC)、氮(TN)等进行了测定分析。[结果
]
①土壤经全冻全融后,沉降分选所得>500 μm和≤125 μm的颗粒含量减少,125~500 μm的颗粒增加;土壤EC在大粒级中较高;SOC和TN在大粒级中(>500 μm)含量降低,在较小粒级(≤125 μm)含量增加。②渐次分层解冻土壤经沉降后,外层(T
1
)≤63 μm颗粒偏少,内层(T
3
)125~500 μm颗粒偏多;盐分和有机碳氮在外层大粒级中含量较高。③全冻全融土壤沉降后,盐分流失率达64.8%,SOC和TN流失率相对较低,为4.08%和2.72%;渐次解冻沉降处理内层(T
3
)土壤盐分和有机质流失程度大于外层(T
1
)。[结论
]
冻融沉降后,外层土壤破碎程度大,坡面土壤颗粒趋向均质化;有机质含量在粒级间差异明显,其在小粒级土壤中分布更加稳定;盐分和有机质在冻融沉降过程中会从土壤内层向外层迁移而造成流失。
[Objective] The classification of sediment particles and the accompanying distribution characteristics of carbon
nitrogen and salt in the process of soil thawing layer by layer under snowmelt runoff scenario were analyzed in order to identify the mechanism of soil freeze-thaw erosion and the induced micro-environmental effects on eroding slopes. [Methods] Soil samples were obtained from an eroding slope in the mollisol region of Northeastern China. Air-dried soil was used to fill columns that were subjected to three treatments: non-freeze-thaw
full freeze-full thaw
and gradual progressive thawing after freezing. The soil columns were completely immersed in a water bath so that thawing occurred from outside to inside. All soil samples were then fractionated by settling velocity
and the electrical conductivity (EC)
pH value
soil organic carbon (SOC)
and total nitrogen (TN) of each particle size were determined and analyzed. [Results] ① The freeze-thaw process reduced the proportion of the soil particles >500 μm and ≤125 μm
but increased the proportion of soil particles between 125 μm and 500 μm. Larger particles had higher EC
but lower SOC and TN. ② Across gradual progressively thawed layers
the outer layer (thawed earlier) had fewer particles ≤63 μm
and the inner layer (thawed later) had more particles between 125 μm and 500 μm. More specifically
EC
SOC
and TN were higher in the larger fractions from the outer layer. ③ Compared with the original soil
64.8% of the dissolved solids were lost from the soil that experienced gradual progressive thawing
but the loss rate of SOC and TN was only 4.08% and 2.72%
respectively. The loss of dissolved solids and organic matter was greater from the inner layer than from the outer layer. [Conclusion] After freezing and thawing
the degree of fragmentation of the outer layer of soil was large
and the soil particles on the slope tended to become homogenized. Organic matter content varied significantly between particle size classes
and its distribution was more stable in small-grained soils. Salts and organic matter migrated from the inner layer of the soil to the outer layer during the freeze-thaw process
resulting in loss.
孙宝洋,李占斌,肖俊波,等.冻融作用对土壤理化性质及风水蚀影响研究进展[J].应用生态学报,2019,30(1):337-347.
Ma Renming, Jiang Yu, Liu Bo, et al. Effects of pore structure characterized by synchrotron-based micro-computed tomography on aggregate stability of black soil under freeze-thaw cycles [J]. Soil and Tillage Research, 2021,207:104855.
张科利,刘宏远.东北黑土区冻融侵蚀研究进展与展望[J].中国水土保持科学,2018,16(1):17-24.
Liu Xinmin, Feng Bo, Tian Rui, et al. Electrical double layer interactions between soil colloidal particles: polarization of water molecule and counterion [J]. Geoderma,2020,380:114693.
Zhai Jinbang, Zhang Ze, Melnikov A,et al. Experimental study on the effect of freeze-thaw cycles on the mineral particle fragmentation and aggregation with different soil types[J]. Minerals, 2021,11(9):913. https://doi.org/10.3390/min11090913
Liu Jianpeng, Yang Ping, Yang Zhaohui. Water and salt migration mechanisms of saturated chloride clay during freeze-thaw in an open system [J]. Cold Regions Science and Technology, 2021,186:103277.
Wang Mengqin, Zhu Yan, Zhao Tianxing, et al. Chemical characteristics of salt migration in frozen soils during the freezing-thawing period [J]. Journal of Hydrology, 2022,606:127403.
崔莉红,朱焱,赵天兴,等.季节性冻融土壤盐分离子组成与冻结层盐分运移规律研究[J].农业工程学报,2019,35(10):75-82.
Liu Tiejun, Xu Xiangtian, Yang Jie. Experimental study on the effect of freezing-thawing cycles on wind erosion of black soil in Northeast China [J]. Cold Regions Science and Technology, 2017,136:1-8.
王伦,郑粉莉,师宏强,等.壤中流和土壤解冻深度对黑土坡面融雪侵蚀的影响[J].应用生态学报,2021,32(12):4177-4185.
Li Guiyuan, Fan Haoming. Effect of freeze-thaw on water stability of aggregates in a black soil of Northeast China [J]. Pedosphere, 2014,24(2):285-290.
Hu Y, Kuhn N J. Aggregates reduce transport distance of soil organic carbon: are our balances correct? [J]. Biogeosciences, 2014,11(22):6209-6219.
Han Zhen, Wang Xiaoyan, Song Dandan, et al. Response of soil erosion and sediment sorting to the transport mechanism on a steep rocky slope [J]. Earth Surface Processes and Landforms, 2019,44(12):2467-2478.
Zhang Shaoliang, Zhang Xingyi, Liu Zhihua, et al. Spatial heterogeneity of soil organic matter and soil total nitrogen in a mollisol watershed of Northeast China [J]. Environmental Earth Sciences, 2014,72(1):275-288.
Edwards L M. The effect of alternate freezing and thawing on aggregate stability and aggregate size distribution of some Prince Edward Island soils [J]. Journal of Soil Science, 1991,42(2):193-204.
胡亚鲜,Nikolaus J.Kuhn.利用土壤颗粒的沉降粒级研究泥沙的迁移与分布规律[J].土壤学报,2017,54(5):1115-1124.
Zhang Ze, Pendin V V, Feng W, et al. The influence of freeze-thaw cycles on the granulometric composition of Moscow morainic clay [J]. Sciences in Cold and Arid Regions, 2015,7(3):199-205.
王恩姮,赵雨森,陈祥伟.季节性冻融对典型黑土区土壤团聚体特征的影响[J].应用生态学报,2010,21(4):889-894.
王风,韩晓增,李良皓,等.冻融过程对黑土水稳性团聚体含量影响[J].冰川冻土,2009,31(5):915-919.
Mueller C W, Schlund S, Prietzel J, et al. Soil aggregate destruction by ultrasonication increases soil organic matter mineralization and mobility [J]. Soil Science Society of America Journal, 2012,76(5):1634-1643.
周旺明,王金达,刘景双,等.冻融对湿地土壤可溶性碳、氮和氮矿化的影响[J].生态与农村环境学报,2008,24(3):1-6.
Qin Yan, Bai Yufeng, Chen Guoshuang, et al. The effects of soil freeze-thaw processes on water and salt migrations in the western Songnen Plain, China [J]. Scientific Reports, 2021,11:3888.
Wu Daoyong, Zhou Xiangyang, Jiang Xingyuan. Water and salt migration with phase change in saline soil during freezing and thawing processes [J]. Groundwater, 2018,56(5):742-752.
Bing Hui, He Ping, Zhang Ying. Cyclic freeze-thaw as a mechanism for water and salt migration in soil [J]. Environmental Earth Sciences, 2015,74(1):675-681.
Liu Bo, Ma Renming, Fan Haoming. Evaluation of the impact of freeze-thaw cycles on pore structure characteristics of black soil using X-ray computed tomography [J]. Soil and Tillage Research, 2021,206:104810.
Plante A F, Conant R T, Stewart C E, et al. Impact of soil texture on the distribution of soil organic matter in physical and chemical fractions [J]. Soil Science Society of America Journal, 2006,70(1):287-296.
0
浏览量
709
下载量
0
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621