Spatio-termporal Characteristics and Pedotransfer of Soil Penetration Resistance in Eroded Sloping Farmland of Black Soil Region, China

XIONG Qian; GAO Lei; PENG Xinhua; QIAN Rui; ZHONG Xuemei; LI Linyuan; LI Qinglin

doi:10.13870/j.cnki.stbcxb.2024.04.019

您当前的位置：

首页 >

文章列表页 >

Spatio-termporal Characteristics and Pedotransfer of Soil Penetration Resistance in Eroded Sloping Farmland of Black Soil Region, China

更新时间：2025-03-12

- Spatio-termporal Characteristics and Pedotransfer of Soil Penetration Resistance in Eroded Sloping Farmland of Black Soil Region, China
- Vol. 38, Issue 4, Pages: 162-169(2024)
- 作者机构：
  
  1. 桂林理工大学地球科学学院,广西,桂林,541004
  2. 中国科学院南京土壤研究所土壤与农业可持续发展国家重点实验室,南京,210008
  3. 中国科学院大学,北京,100049
- 作者简介：
- 基金信息：
- DOI：10.13870/j.cnki.stbcxb.2024.04.019
  CLC： S157.1
- Published：2024
- 稿件说明：
移动端阅览
XIONG Qian, GAO Lei, PENG Xinhua, et al. Spatio-termporal Characteristics and Pedotransfer of Soil Penetration Resistance in Eroded Sloping Farmland of Black Soil Region, China[J]. 2024, 38(4): 162-169.
DOI：

XIONG Qian, GAO Lei, PENG Xinhua, et al. Spatio-termporal Characteristics and Pedotransfer of Soil Penetration Resistance in Eroded Sloping Farmland of Black Soil Region, China[J]. 2024, 38(4): 162-169. DOI： 10.13870/j.cnki.stbcxb.2024.04.019.

摘要

[目的] 为探明侵蚀坡耕地黑土硬度的时空特征及关键驱动因素。[方法] 基于典型水蚀坡耕地110个样点土壤穿透阻力动态监测及其相关因素的测定

在阐明土壤穿透阻力时空特征的基础上

利用多元线性回归(MLR)和随机森林(RFR)模型分析土壤穿透阻力的影响因素

并进一步构建其传递函数。[结果] 土壤穿透阻力时空变异性受土层深度、水分条件及农事活动等因素的综合影响

耕作层土壤穿透阻力空间上的异质性显著低于亚表层

变异系数分别为17.4%和26.3%。随土壤由湿变干和距离翻耕的时间增加

空间异质性呈增强趋势。土壤侵蚀影响土壤穿透阻力

强烈侵蚀区土壤穿透阻力高于沉积区

特别是在湿润条件下

差异更为显著(p<0.05)。与自然林地相比

所研究坡耕地73%样点的土壤穿透阻力增加

尤其在强侵蚀区。土壤含水量、容重和有机碳(SOC)是土壤穿透阻力的主要影响因素

Pearson系数分别为-0.69

0.58

-0.54

三者共同解释土壤穿透阻力88%的变异。RFR模型在土壤穿透阻力预测中表现优于MLR模型

在生长季均值的预测中

R2可达0.91

RMSE仅为91.2 kPa。[结论] 研究结果加深对侵蚀背景下黑土硬度空间分异特征的理解

为黑土压实管控提供理论依据。

Abstract

[Objective] To delve deeper into the spatiotemporal characteristics and pivotal driving factors underlying the hardness of black soil in eroded sloping farmlands. [Methods] Based on the dynamic monitoring of soil penetration resistance across 110 sample points in typical water erosion sloping farmlands

coupled with measurements of pertinent factors

the factors affecting soil penetration resistance were analyzed by multivariate linear regression (MLR) and random forest (RFR) models

and its transfer function was further construct. [Results] The spatiotemporal variability of soil penetration resistance was influenced by a combination of soil depth

moisture conditions

and agricultural practices. Notably

the spatial heterogeneity was significantly lower in the topsoil layer compared to the sub-surface layer

with coefficients of variation of 17.4% and 26.3%

respectively. As the soil dried out and the duration since the last tillage increases

spatial heterogeneity tended to intensify. Soil erosion played a significant role

with higher soil penetration resistance observed in areas of intense erosion compared to deposition zones

particularly under wet conditions where the difference is most pronounced (p<0.05). Furthermore

73% of the sampled points in the studied sloping farmlands exhibited increased soil penetration resistance compared to natural forestlands

especially in regions of intense erosion. Key factors that influenced soil penetration resistance included soil moisture content

bulk density

and soil organic carbon (SOC)

with Pearson coefficients of -0.69

0.58 and -0.54

respectively

collectively explaining 88% of its variability. In terms of predictive soil penetration resistance

the RFR model demonstrated superior accuracy compared to the MLR model

achieving an R2 of 0.91 and an RMSE of 91.2 kPa for mean predictions across the growing season. [Conclusion] This study enhances our understanding of the spatial heterogeneity characteristics of black soil hardness under erosion

providing a theoretical foundation for effective management of soil compaction in black soil regions.

关键词

Keywords

references

MONTANARELLA L, CHUDE V, YAGI K, et al. Status of the World’s Soil Resources (SWSR) -Main Report[M]. Rome:Food and Agriculture Organization of the United Nations,2015.

ROBINSON D A, HOCKLEY N, COOPER D M, et al. Natural capital and ecosystem services, developing an appropriate soils framework as a basis for valuation[J].Soil Biology and Biochemistry,2013,57:1023-1033.

石彦琴,陈源泉,隋鹏,等.农田土壤紧实的发生、影响及其改良[J].生态学杂志,2010,29(10):2057-2064. SHI Y Q, CHEN Y Q, SUI P, et al. Cropland soil compaction: Its causes, influences, and improvement[J].Chinese Journal of Ecology,2010,29(10):2057-2064.

李勇,赵云泽,勾宇轩,等.黄淮海旱作区农田耕层土壤结构特征与其影响因素[J].农业机械学报,2022,53(3):321-330. LI Y,ZHAO Y Z, GOU Y X, et al. Characteristics and influencing factors of topsoil structure of farmland in dry farming region of Huang-Huai-Hai[J].Transactions of the Chinese Society for Agricultural Machinery,2022,53(3):321-330.

TANG C S, GONG X P, SHEN Z T, et al. Soil micro-penetration resistance as an index of its infiltration processes during rainfall[J].Journal of Rock Mechanics and Geotechnical Engineering,2022,14(5):1580-1587.

黄怡婷,陈俊熹,高钰淏,等.长期耕作对典型黑土水力性质的影响[J].土壤学报,2024,61(4):998-1008. HUANG Y T, CHEN J X, GAO Y H, et al. Effects of long-term tillage on hydraulic properties of typical black soil [J].Acta Pedologica Sinica,2024,61(4):998-1008.

杨文苑.土壤容重和水分对典型黑土穿透阻力及玉米生长的影响.兰州:甘肃农业大学,2023. YANG W Y. Effects of soil bulk density and moisture on penetration resistance of typical mollisols and growth of maize .Lanzhou: Gansu Agricultural University,2023.

张兴义,刘晓冰.中国黑土研究的热点问题及水土流失防治对策[J].水土保持通报,2020,40(4):340-344. ZHANG X Y, LIU X B. Key issues of mollisols research and soil erosion control strategies in China[J].Bulletin of Soil and Water Conservation,2020,40(4):340-344.

FERNANDES M M H, COELHO A P, DA SILVA M F, et al. Estimation of soil penetration resistance with standardized moisture using modeling by artificial neural networks[J].Catena, 2020,189:e104505.

SOUZA R, HARTZELL S, FREIRE FERRAZ A P, et al. Dynamics of soil penetration resistance in water-controlled environments[J].Soil and Tillage Research,2021,205:e104768.

ZHANG H, WU P B, YIN A J, et al. Prediction of soil organic carbon in an intensively managed reclamation zone of Eastern China: A comparison of multiple linear regressions and the random forest model[J].The Science of the Total Environment,2017,592:704-713.

宋志廷,赵玉杰,周其文,等.基于地质统计及随机模拟技术的天津武清区土壤重金属源解析[J].环境科学,2016,37(7):2756-2762. SONG Z T, ZHAO Y J, ZHOU Q W, et al. Applications of geostatistical analyses and stochastic models to identify sources of soil heavy metals in Wuqing district, Tianjin, China[J].Environmental Science,2016,37(7):2756-2762.

韩晓增,邹文秀.东北黑土地保护利用研究足迹与科技研发展望[J].土壤学报,2021,58(6):1341-1358. HAN X Z, ZOU W X. Research perspectives and footprint of utilization and protection of black soil in Northeast China[J].Acta Pedologica Sinica,2021,58(6):1341-1358.

李林源,高磊,彭新华,等.典型水蚀区坡耕地黑土质量的空间分异特征及影响因素[J].水土保持学报,2024,38(3):382-390,399. LI L Y, GAO L, PENG X H, et al. Spatial variation characteristics and influencing factors of black soil quality in typical water-eroded sloping croplands[J].Journal of soil and Waterconservation, 2024,38(3):382-390,399.

鲍士旦.土壤农化分析[M].北京:中国农业出版社,2000. BAO S D. Soil agrochemical analysis[M].Beijing: China Agricultare Press,2000.

寇青青,运剑苇,汪明星,等.渝东北紫色土饱和导水率传递函数研究[J].土壤,2020,52(3):611-617. KOU Q Q, YUN J W, WANG M X, et al. Study on pedotransfer function of saturated hydraulic conductivity of purple soil in northeast Chongqing[J].Soils,2020,52(3):611-617.

尹炳,汪建飞,师胜,等.矿业废弃地复垦土壤-作物硒吸收特征及其对重金属拮抗效应[J].环境科学,2020,41(4):1904-1913. YIN B, WANG J F, SHI S, et al. Selenium uptake characteristics of reclaimed soil-crop from mining wasteland and its antagonistic effects on heavy metals[J].Environmental Science,2020,41(4):1904-1913.

脱登峰. 黄土高原水蚀风蚀交错区土壤退化机理研究.陕西杨凌:西北农林科技大学,2016. TUO D F. The study of the soil degradation mechanism in wind-water erosion crisscross region on the Loess Plateau.Yangling, Shaanxi: Northwest A&F University,2016.

李雪亮,张晴雯,李孟妮,等.黑土长缓坡地形与横垄对土壤有机碳空间分异的交互作用[J].农业工程学报,2024,40(3):103-113. LI X L, ZHANG Q W, LI M N, et al. Interaction between long gently sloping topography and contour-ridge on the spatial partitioning of soil organic carbon in a black soil[J].Transactions of the Chinese Society of Agricultural Engineering,2024,40(3):103-113.

RÜCKNAGEL J, RADEMACHER A, GÖTZE P, et al. Uniaxial compression behaviour and soil physical quality of topsoils under conventional and conservation tillage[J].Geoderma,2017,286:1-7.

韩巍,徐晓旭,李冬,等.耕作方式对辽西褐土区土壤穿透阻力的影响及机理[J].水土保持学报,2020,34(6):143-149. HAN W, XU X X, LI D, et al. Effects of tillage methods on soil penetration resistance and its mechanism in the cinnamon soil area of western Liaoning Province[J].Journal of Soil and Water Conservation,2020,34(6):143-149.

GAO L, SHAO M G. Temporal stability of soil water storage in diverse soil layers[J].Catena,2012,95:24-32.

李勇,赵云泽,勾宇轩,等.黄淮海旱作区土壤压实度空间分布特征及其影响因素[J].农业工程学报,2021,37(13):83-91. LI Y, ZHAO Y Z, GOU Y X, et al. Spatial distribution characteristics and influence factors of degree of compaction in dry-farming Huang-Huai-Hai Plain of China[J].Transactions of the Chinese Society of Agricultural Engineering,2021,37(13):83-91.

LONGEPIERRE M, WIDMER F, KELLER T, et al. Limited resilience of the soil microbiome to mechanical compaction within four growing seasons of agricultural management[J].ISME Communications,2021,1:e44.

郑粉莉,张加琼,刘刚,等.东北黑土区坡耕地土壤侵蚀特征与多营力复合侵蚀的研究重点[J].水土保持通报,2019,39(4):314-319. ZHENG F L, ZHANG J Q, LIU G, et al. Characteristics of soil erosion on sloping farmlands and key fields for studying compound soil erosion caused by multi-forces in mollisol region of Northeast China[J].Bulletin of Soil and Water Conservation,2019,39(4):314-319.

高晨.基于拖拉机行走的黑土压实模拟.南京:中国科学院南京土壤研究所,2023. GAO C. Black soil compaction simulation based on tractor walking.Nanjing: Institute of Soil Science, Chinese Academy of Sciences,2023.

高冰可.红壤穿透阻力的影响因素与预测模型.武汉:华中农业大学,2014. GAO B K. Influencing factors and prediction model on red soil penetration resistance . Wuhan:Huazhong Agricultural University,2014.

Views

25353

下载量

CSCD

Alert me when the article has been cited

提交

Tools

Publicity Resources

Impacts of Slope Erosion-Deposition Processes on Soil Organic Carbon Fractions in Black Soil Region of Northeast China

Response of Soil Stoichiometric to Soil Erosion on Slope Farmland in Black Soil Region of Northeast China

Effects of Crushed Corn Straw Returning on Soil Erosion Characteristics at the Black Soil Hillslopes

Small Watershed Erosion Model （SWEM）

Multi-Temporal-Scale Variation Characteristics of Canopy Conductance in Artificial Shrubland Ecosystems and Its Biophysical Driving Mechanisms

Related Author

ZHOU Xiao

WANG Bin

FAN Hua

WANG Wengang

TONG Yaning

WANG Jun

LI Liguo

KANG Xiaoqi

Related Institution

School of Soil and Water Conservation， Beijing Forestry University

Jinyun Mountain Three-Gorges Reservoir Area （Chongqing） Forest Ecosystem Research Station， Beijing Forestry University

Heilongjiang Province Key Laboratory of Soil and Water Conservation， Heilongjiang Province Hydraulic Research Institute

State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, College of Soil and Water Conservation Science and Engineering, Northwest A&F University, Yangling

Institute of Soil and Water Conservation, Chinese Academy of Sciences, Ministry of Water Resources, Yangling

⁰