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Spatial distribution of theoretical soil macropores on a continental scale and its eco-hydrological significance in China

  • Soils, Sec 2 • Global Change, Environ Risk Assess, Sustainable Land Use • Research Article
  • Published:
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Abstract

Purpose

Soil macropores affect the proportion of rainfall infiltration and regulate the amount of water available to the plants on a field scale. However, the distribution of soil macropores and the effect on hydrologic and ecological regimes have been underestimated at a continental scale. The aim of this study was to investigate the relationships between soil properties and climatic factors on soil macropores and assess the eco-hydrological effect of soil macropores.

Materials and methods

We hypothesized that the spatial distribution of soil macropores was controlled by soil properties and climatic factors at the continental scale. Using a spatial error-egression method, the soil effective porosity (EP) and residual effective porosity (REP) across China were calculated. The effects of soil macropores on soil physicochemical properties and climate factors were analyzed by the random forest model. The effect of macropores on soil water content (SWC) and normalized difference vegetation index (NDVI) was also analyzed.

Results and discussion

The EP ranged from 0.06 to 0.35 cm3 cm−3 and was significantly related with soil chemical index, particularly, negatively correlated with cation exchange capacity (CEC) and total nitrogen (TN), but positively correlated with pH. There was a negative relationship between REP and mean annual precipitation in drylands. In humid regions, there was a positive relationship between REP and mean annual precipitation. Random forest model showed in humid region mean annual precipitation was more important than the annual temperature difference in explaining REP, but the results were reversed in drylands. The SWC and NDVI had different correlations with REP in drylands and humid regions.

Conclusion

Soils with better quality had lower EP at the continental scale. Soil macropores were related simultaneously to precipitation and temperature conditions. Importantly, soil macropores were not conducive to soil water conservation and vegetation development in drylands.

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Data availability

The authors declare that the majority of the data supporting the findings of this study are available through the links given in the paper. The unpublished data used in this paper can be available from W. R. Kang (kangwenrong@nieer.ac.cn) upon request.

Abbreviations

EP:

Effective porosity

REP:

Residual effective porosity

SWC:

Soil water content

NDVI:

Normalized differential vegetation index

CEC:

Cation exchange capacity

TN :

Total nitrogen

TP :

Total phosphorous

TK :

Total potassium

AN :

Alkali-hydrolysable nitrogen

AP:

Available phosphorous

AK:

Available potassium

H:

Exchangeable H+

AL:

Exchangeable Al3+

CA:

Exchangeable Ca2+

MG :

Exchangeable Mg2+

K :

Exchangeable K+

References

  • Alakukku L, Nuutinen V, Ketoja E, Koivusalo H, Paasonen-Kivekäs M (2010) Soil macroporosity in relation to subsurface drain location on a sloping clay field in humid climatic conditions. Soil Till Res 106:275–284

    Article  Google Scholar 

  • Anselin L (2005) Exploring spatial data with GeoDaTM: A workbook. Center for Spatially Integrated Social Science

  • Benito P, Bortolotti V, Fornasari G, Vannini M (2016) Evaluation of effect of soil organic matter on pores by 1H time-domain magnetic resonance relaxometry and adsorption - desorption of N2. Eur J Soil Sci 67:314–323

    Article  CAS  Google Scholar 

  • Bodner G, Scholl P, Kaul HP (2013) Field quantification of wetting–drying cycles to predict temporal changes of soil pore size distribution. Soil Till Res 133:1–9

    Article  CAS  Google Scholar 

  • Bolan N, Kandaswamy K (2004) Encyclopedia of soils in the environment, edited by D. Hillel. Academic Press, New York, pp.196–202

  • Bronick CJ, Lal R (2004) Soil structure and management: a review. Geoderma 124:3–32

    Article  ADS  Google Scholar 

  • Caplan JS, Giménez D, Hirmas DR, Brunsell NA, Knapp AK (2019) Decadal-scale shifts in soil hydraulic properties as induced by altered precipitation. Sci Adv 5

  • Caplan JS, Giménez D, Subroy V, Heck RJ, Prior SA, Runion GB, Torbert HA (2017) Nitrogen-mediated effects of elevated CO2 on intra-aggregate soil pore structure. Glob Chang Biol 23:1585–1597

    Article  PubMed  ADS  Google Scholar 

  • Coquard J, Duffy PB, Taylor KE (2004) Present and future surface climate in the western USA as simulated by 15 global climate models. Clim Dynam 23:455–472

    Article  ADS  Google Scholar 

  • Dai Y, Shangguan W, Duan Q, Liu B, Fu S, Niu G (2013) Development of a China dataset of soil hydraulic parameters using pedotransfer functions for land surface modeling. J Hydrometeorol 14:869–887

    Article  ADS  Google Scholar 

  • Dash JG, Rempel AW, Wettlaufer JS (2006) The physics of premelted ice and its geophysical consequences. Rev Mod Phys 78:695–741

    Article  CAS  ADS  Google Scholar 

  • Deurer M, Sivakumaran S, Ralle S, Vogeler I, McIvor I, Clothier B, Green S, Bachmann J (2009) The impact of soil carbon management on soil macropore structure: a comparison of two apple orchard systems in New Zealand. Eur J Soil Sci 60:945–955

    Article  CAS  Google Scholar 

  • Dorigo WA, Gruber A, De Jeu RA, Wagner W, Stacke T, Loew A, Kidd R (2015) Evaluation of the ESA CCI soil moisture product using ground-based observations. Remote Sens Environ 162:380–395

  • Es HM, Ogden CB, Hill RL, Schindelbeck RR, Tsegaye T (1999) Integrated assessment of space, time, and management-related variability of soil hydraulic properties. Soil Sci Soc Am J 63:1599–1608

    Article  Google Scholar 

  • Evans J, Geerken R (2004) Discrimination between climate and human-induced dryland degradation. J Arid Environ 57:535–554

    Article  Google Scholar 

  • Feng Y, Wang J, Bai Z, Reading L, Jing Z (2020) Three-dimensional quantification of macropore networks of different compacted soils from opencast coal mine area using x-ray computed tomography. Soil Till Res 198:104567

  • Filipović V, Defterdarović J, Šimůnek J, Filipović L, Ondrašek G, Romić D (2020) Estimation of vineyard soil structure and preferential flow using dye tracer, x-ray tomography, and numerical simulations. Geoderma 380:114699

    Article  ADS  Google Scholar 

  • Geerken R, Ilaiwi M (2004) Assessment of rangeland degradation and development of a strategy for rehabilitation. Remote Sens Environ 90:490–504

    Article  ADS  Google Scholar 

  • Hayashi Y, Ken,ichirou K, Mizuyama T (2006) Changes in pore size distribution and hydraulic properties of forest soil resulting from structural development. J Hydrol 331:85–102

  • Hirmas DR, Giménez D, Nemes A, Kerry R, Brunsell NA, Wilson CJ (2018) Climate-induced changes in continental-scale soil macroporosity may intensify water cycle. Nature 561:100–103

    Article  CAS  PubMed  ADS  Google Scholar 

  • Hlaváčiková H, Holko L, Danko M, Novák V (2019) Estimation of macropore flow characteristics in stony soils of a small mountain catchment. J Hydrol 574:1176–1187

    Article  Google Scholar 

  • Huang J, Guan X, Ji F (2012) Enhanced cold-season warming in semi-arid regions. Atmos Chem Phys 12:5391–5398

    Article  CAS  ADS  Google Scholar 

  • Hussain SI, Phillips LA, Hu Y, Frey SK, Geuder DS, Edwards M, Blowes DW (2021) Differences in phosphorus biogeochemistry and mediating microorganisms in the matrix and macropores of an agricultural clay loam soil. Soil Biol Biochem 161:108365

    Article  CAS  Google Scholar 

  • Isabona J, Imoize AL, Kim Y (2022) Machine learning-based boosted regression ensemble combined with hyperparameter tuning for optimal adaptive learning. Sensors 22(10):3776

    Article  PubMed  PubMed Central  ADS  Google Scholar 

  • Jaggi IK, Gorantiwar SM, Khanna SS (1972) Effect of bulk density and aggregate size on wheat growth. J Indian Soc Soil Sci 20:421–423

    Google Scholar 

  • Juarez S, Nunan N, Duday AC, Pouteau V, Schmidt S, Hapca S, Chenu C (2013) Effects of different soil structures on the decomposition of native and added organic carbon. Eur J Soil Biol 58:81–90

    Article  CAS  Google Scholar 

  • Köhne JM, Mohanty BP, Simůnek J (2006) Inverse dual-permeability modeling of preferential water flow in a soil column and implications for field-scale solute transport. Vadose Zone J 5:59–76

    Article  Google Scholar 

  • Konert M, Vandenberghe JEF (1997) Comparison of laser grain size analysis with pipette and sieve analysis: a solution for the underestimation of the clay fraction. Sedimentology 44:523–535

    Article  CAS  ADS  Google Scholar 

  • Kravchenko AN, Negassa WC, Guber AK, Rivers MK (2015) Protection of soil carbon within macro-aggregates depends on intra-aggregate pore characteristics. Sci Rep 5:16261

    Article  CAS  PubMed  PubMed Central  ADS  Google Scholar 

  • Lacroix EM, Rossi RJ, Bossio D, Fendorf S (2021) Effects of moisture and physical disturbance on pore-scale oxygen content and anaerobic metabolisms in upland soils. Sci Total Environ 780:146572

  • Li K, Li Q, Liu C (2022) Effect of freezing temperature and water content on pore structure characteristics of coastal saline-alkali soil under frost heave. J Soils Sediments 22:1819–1827

    Article  Google Scholar 

  • Lohse KA, Dietrich WE (2005) Contrasting effects of soil development on hydrological properties and flow paths. Water Resour Res 41:W12419

    Article  ADS  Google Scholar 

  • Luo L, Lin H, Li S (2010) Quantification of 3-D soil macropore networks in different soil types and land uses using computed tomography. J Hydro 393:53–64

    Article  Google Scholar 

  • Mekala C, Nambi IM (2017) Understanding the hydrologic control of N cycle: effect of water filled pore space on heterotrophic nitrification, denitrification and dissimilatory nitrate reduction to ammonium mechanisms in unsaturated soils. J Contam Hydrol 202:11–22

    Article  CAS  PubMed  Google Scholar 

  • Melissa AC, Christopher WS, Nate GM, William TP, Aimée TC (2012) Response of the soil microbial community to changes in precipitation in a semiarid ecosystem. Appl Environ Microbiol 78:8587–8594

  • National Soil Survey Office (1996) China soil species description (in Chinese). China Agric. Press, Beijing, vol. 1–6

  • Pinault JL, Amraoui N, Golaz C (2005) Groundwater-induced flooding in macropore-dominated hydrological system in the context of climate changes. Water Resour Res 41:w05001

    Article  ADS  Google Scholar 

  • Qian P, Schoenaru JJ, Karamanos RE (1994) Simultaneous extraction of available phosphorus and potassium with a new soil test: a modification of Kelowna extraction. Commun Soil Sci Plant Anal 25:627–635

    Article  CAS  Google Scholar 

  • R Core Team (2023) R: A language and environment for statistical computing. R Foundation for Statistical Computing. https://www.R-project.org/

  • Rawls WJ, Giménez D, Grossman R (1998) Use of soil texture, bulk density, and slope of the water retention curve to predict saturated hydraulic conductivity. Trans ASAE 41:983–988

    Article  Google Scholar 

  • Shangguan W, Dai Y, Liu B, Ye A, Yuan H (2012) A soil particle-size distribution dataset for regional land and climate modelling in China. Geoderma 171:85–91

    Article  ADS  Google Scholar 

  • Shen X, An R, Quaye-Ballard JA, Zhang L, Wang Z (2016) Evaluation of the European Space Agency climate change initiative soil moisture product over China using variance reduction factor. J Am Water Resour Assoc 52:1524–1535

    Article  Google Scholar 

  • Smith AP, Bond-Lamberty B, Benscoter BW, Tfaily MM, Hinkle CR, Liu C, Bailey VL (2017) Shifts in pore connectivity from precipitation versus groundwater rewetting increases soil carbon loss after drought. Nat Commun 8:1–11

    Article  Google Scholar 

  • Soon YK, Abboud S (1991) A comparison of some methods for soil organic carbon determination. Commun Soil Sci Plant Anal 22:943–954

    Article  CAS  Google Scholar 

  • Stanley EH, Rojas Salazar S, Lottig NR, Schliep EM, Filstrup CT, Collins SM (2019) Comparison of total nitrogen data from direct and Kjeldahl-based approaches in integrated data sets. Limnol Oceanogr Methods 17:639–649

    Article  Google Scholar 

  • Sullivan PL, Billings SA, Hirmas D, Li L, Zhang X, Ziegler S, Wen H (2022) Embracing the dynamic nature of soil structure: a paradigm illuminating the role of life in critical zones of the Anthropocene. Earth-Sci Rev 225:103873

    Article  CAS  Google Scholar 

  • Surajit M, Debashis C (2022) Global meta-analysis suggests that no-tillage favorably changes soil structure and porosity. Geoderma 405:115443

    Article  Google Scholar 

  • Wang M, Xu S, Yang J, Xu L, Yu Q, Xie X, Shi X, Zhao Y (2021a) The effect of organic and conventional management practices on soil macropore structure in greenhouse vegetable production. Eur J Soil Sci 72:2133–2149

    Article  Google Scholar 

  • Wang T, Wu T, Wang P, Li R, Xie C, Zou D (2018) Spatial distribution and changes of permafrost on the Qinghai-Tibet Plateau revealed by statistical models during the period of 1980 to 2010. Sci Total Environ 650:661–670

    Article  PubMed  ADS  Google Scholar 

  • Wang Z, Wu Y, Cao Q, Shen Y, Zhang B (2021) Modeling the coupling processes of evapotranspiration and soil water balance in agroforestry systems. Agric Water Manag 250:106839

  • Watson KW, Luxmoore RJ (1986) Estimating macroporosity in a forest watershed by use of a tension infiltrometer1. Soil Sci Soc Am J 50:578–582

  • Xu X, Xin P, Zhou T, Yu X (2023) Effects of large macropores on saline water evaporation from marsh soil. Water Resour Res 59:e2022WR033276

  • Yao T, Zhang W, Gulaqa A, Cui Y, Zhou Y, Weng W, Jin F (2021) Effects of peanut shell biochar on soil nutrients, soil enzyme activity, and rice yield in heavily saline-sodic paddy field. J Soil Sci Plant Nutr 21:655–664

    Article  CAS  Google Scholar 

  • Zhang Y, Zhao W, He J, Fu L (2018) Soil susceptibility to macropore flow across a desert-oasis ecotone of the Hexi Corridor, Northwest China. Water Resour Res 54:1281–1294

    Article  ADS  Google Scholar 

  • Zhang Y, Zhao W, Li X, Jia A, Kang W (2021) Contribution of soil macropores to water infiltration across different land use types in a desert–oasis ecoregion. Land Degrad Dev 32:1751–1760

    Article  Google Scholar 

  • Zhao L, Ping C, Yang D, Cheng G, Ding Y, Liu S (2004) Changes of climate and seasonally frozen ground over the past 30 years in Qinghai-Xizang (Tibetan) Plateau, China. Glob Planet Change 43:19–31

    Article  ADS  Google Scholar 

  • Zhou M, Liu C, Wang J, Meng Q, Yuan Y, Ma X, Du W (2020) Soil aggregates stability and storage of soil organic carbon respond to cropping systems on black soils of Northeast China. Sci Rep 10:265

    Article  CAS  PubMed  PubMed Central  ADS  Google Scholar 

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Acknowledgements

We thank the reviewers and editors for their constructive comments on this manuscript. We sincerely thank Dr. Jeffery Hannah of Michigan State University for her help with English language and grammar editing.

Funding

This study was supported by the National Natural Science Foundation of China (No. 42071044, 42230720), the Youth Innovation Promotion Association CAS (No. 2020420), and Top Talents (Science and Technology) Program of Gansu Province (No. E339040101).

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Conceptualization: Wenrong Kang, Yongyong Zhang, and Wenzhi Zhao; methodology: Wenrong Kang, Yongyong Zhang, and Shaoxiong Wu; writing—original draft: Wenrong Kang and Yongyong Zhang; review and editing: Yongyong Zhang and Shaoxiong Wu; funding acquisition and supervision: Yongyong Zhang. All authors read and approved the final submission of the manuscript.

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Correspondence to Yongyong Zhang.

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Wenrong Kang, Shaoxiong Wu, and Wenzhi Zhao are co-authors.

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Kang, W., Zhang, Y., Wu, S. et al. Spatial distribution of theoretical soil macropores on a continental scale and its eco-hydrological significance in China. J Soils Sediments 24, 563–574 (2024). https://doi.org/10.1007/s11368-023-03652-2

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