Greener Journal of Soil Science and Plant Nutrition

Open Access

Nweke and Ijeh

Greener Journal of Soil Science and Plant Nutrition Vol. 4 (4), pp. 036-045, November 2017.

  © 2017 Greener Journals

Research Paper

Manuscript Number: 102517158


(DOI: http://doi.org/10.15580/GJSSPN.2017.4.102517158)

 

Relationship between Aggregate Stability Indices of Four Contrasting Textural Classes of Soils as Influenced by different Periods of Soaking

 

Nweke I.A.*1 and Ijeh A.C.2

 

1Department of Soil Science Chukwuemeka Odumegwu Ojukwu University, Anambra State.

2Nwafor Orizu College of Education Nsugbe Anambra State.

Abstract


The ability of soil aggregates to resist the forces of water and/or wind, the potential to degrade, crust and/or seal is referred to aggregate stability. Little is known about the effect of soil texture and period of soaking on aggregate stability for cultivated soil of four major textural classes in southeast, Nigeria which was the objective of our study. Soil samples representing a range of agricultural soils of four contrasting textural classes of sandy loam; sandy clay loam; clay loam and loam under five different period of soaking namely; 0, 30, 60, 90 and 120 minutes were studied using wet and dry sieve techniques. The indices evaluated include; mean weight diameter wet and dry, water stable aggregates >2.00mm (WSA1); water stable aggregates 2.00mm – 1.00mm (WSA2); water stable aggregates 1.00mm – 0.5mm (WSA3); 0.5mm – 0.25mm (WSA4);  < 0.25 mm (WSA5).  Results generated from the study showed that the studied soil types are poor in organic carbon (OC), organic matter and sodium (Na) contents. Their cation exchange capacity (CEC) values are of moderate values of which ranged from 4.67 – 8.80 cmolkg-1. The relationship study indicated that WSA1 correlated significantly and positively with WSA2 and mean weight diameter wet (MWDW), but negatively with WSA4 and WSA5 with r values of -0.306 and -0.695 respectively. WSA2 was observed to have significant positive correlation with WSA3, WSA4 and MWDW. WSA3 and WSA4 did not correlate significantly with MWDW but has positive correlation with each other with r value of 0.794. WSA5 was found to correlate significantly but negatively withWSA1 – WSA5 (2.00mm – 0.25mm). Mean weight diameter of wet aggregates correlated positively and significantly with degree of aggregation (DA) and state of aggregation (SA) at 0 – 120 minutes, this result was equally true for DA and SA correlation result at times studied. The correlation matrix of mean weight diameter of dry aggregates (MWDD) with MWDW, DA and SA indicated negative correlation in all the time studied, except at 30 minutes where it showed positive correlation with DA with r value of 0.639 and at 90 minutes were it was not significant with DA and SA. The correlation between aggregate stability indices studied and Na, CEC at various periods of soaking was not significant and OM content was low. Though not statistically significant, hydraulic conductivity (HC) and bulk density (BD) showed positive correlation with MWDW, DA and SA in all the soaking period while field capacity (FC) and total porosity (TP) showed negative correlation but not statistically significant with MWDW, DA and SA, but has positive correlation with MWDD. The findings from this study is of evidence that the period of soaking had some contributions to the stability of soil aggregates and soil properties especially with the trend in the correlation matrix between MWDD and MWDW, DA and SA.

 

Keywords: Aggregate stability, water stable aggregates, aggregate sizes, soaking period.


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References


Adesondun JK, Mbagwu JSC, Oti N, (2001). Structural and carbohydrate contents of an ultisol under   different management systems, Soils and Tillage Research 60: 135-142.

 

Amezketa E, (1999). Soil aggregate stability: A review, J. Sustainable Agric. 14: 83-151

 

Anabi M, Houot S, Fracou C, Poitrenandi M, Bissonnais YL, (2008). Soil aggregate stability improvement with urban compost of different materials, Soil Sci. Soc. Am. J. 71: 413-123

 

Asadu CLA, (1992). Environmental impact assessment studies final report on socioeconomic, cultural, health and soil productivity aspects 14th August 1992; Department of Soil Science University of Nigeria, Nsukka

 

Asadu CLA, (2002) comparative evaluation of the contributions of soil physiochemical properties to variation in the yield of four major staple food crops in eastern Nigeria, Soil and Tillage Research 65: 141-155

 

Bazzoffi P, Mbagwu JSC (1986). A structural stability ranking of some soil from north central Italy by water stability index and sixteen other indices, Istituto Sperimontale Studio. C. Difeesa Suolo Firenze, Amali, xvii: 89-98

 

Blake P (1986). Bulk density: In Black C A (ed) Methods of soil analysis Agronomy manual No. 9 part 1 American Society of Agronomy, Madison, WI, USA

 

Bouyoucous GH (1951). A calibration of hydrometer method for making mechanical analysis of soil, Agronomy Journal 43: 434-438.

 

Burkke W, Gabriel’s D, Bourma J (1986) Soil Structure AA Balkema publishers The Netherlands

 

Chisci G, Bazzoffi P, Mbagwu JSC (1989). Comparison of aggregate stability indices for soil classification and assessment of soil management practices, Soil Technology 2: 113-133

 

Denef K, Six J, Merks R, Pausitan K, (2004). Carbon sequestration in micro aggregates, Soil Sci. Soc. Am. J. 58: 1935-1994.

 

 Denef K, Six J, Pausitan K, Merckx R (2001). Importance micro aggregates dynamics in controlling soil carbon stabilization: short term effects of physical disturbance inducing by dry wet cycle, Soil Biol. Biochem. 33: 2145-2153.

 

Dexter AR, (1988). Advances in characterization of soil structure Soil Till. Res. 11: 199-238.

 

Diaz-Zorita M, Perfect E, Grove JH, (2002) Disruptive methods for assessing soil structure, Soil Till. Res. 64: 3-22

 

Evanylo G, McGuinn R, (2000). Agricultural management practices and soil quality; measuring, assessing and comparing laboratory and field test kit indicators of soil quality attribute, Virginia Polytechnic Institute and State University pp 8

 

Eynard A, Schumacher TE, Lindstrom MJ, Malo DD, Kohl RA, (2004). Wet ability of soil aggregates from cultivated and uncultivated Ustolls and Usterns, Aust. J. Soil Res. 42: 163-170.

 

Frankel H, Goertzen JO, Rhoades JD (1978). Effect of clay types and content exchangeable sodium percentage and electrolyte and concentration on clay dispersion and hydraulic conductivity, Soil Sci. Soc. Am. J. 42: 32-39

 

Grieve IC (1980). The magnitude and significance of soil structural stability declines under cereal cropping CATENA 7: 79-85

 

Holeplass H, Singh BR, Lal R, (2004). Carbon Sequestration in soil aggregates under different crop rotations and nitrogen fertilization in an inceptisol in southeastern Norway. Nutrient Cycl. Agroecosys. 70: 167-177.

 

Igwe CA, Akamigbo FOR, Mbagwu JSC (1999). Chemical and mineralogical properties of soils in southeastern, Nigeria in relation to aggregate stability. Geoderma 92: 111-123

 

Jackson ML (1958). Soil chemical analysis Prentice Hall Inc. Englewood Cliff, New York

 

Kay BD, Munkholm LJ, (2004). Management induced soil structure degradation, organic matter depletion and tillage; In : Schjonning P, Elmholt S, Christensen BT (eds) Managing soil quality: challenges in modern Agriculture, CABI publication, Wallingford UK pp185-197.

 

Kemper WD, Chepil WS (1965). Size distribution of aggregates: In methods of soil analysis part 2 CA Black (ed) American Society of Agronomy Madison Wisconsin, pp499-510

 

Khurshid K, Iqbal M, Arif MS, Nawaz A, (2006). Effect of tillage and mulch on soil physical properties and growth of maize. J. Agric. Biol. 8: 593-596.

 

Lal R (1991) Soil structure and sustainability, J. Sustain. Agric. 1: 67-92.

 

Madari B, Pedrol L, Machado DA, Torres E, (2005). No tillage and crop rotation effects on soil aggregation and organic carbon in a Rhodic Ferrasol from southern Brazil, Soil Till. Res. 80: 1985-2000

 

Matkin EA, Smart P (1987). A comparison of test structural stability, Journal of Soil Science 38: 123-135.

 

Mbagwu JSC (1992). A comparison of three micro aggregation indices with other tests of structural stability. Int. Agrophysics 6:27-32

 

Mbagwu JSC (1993). Testing the fit of selected infiltration models on soils with different land use histories. Internal report No IC/93/290, International centre for theoretical physics Trieste, Italy

 

Miquel RJ Norton DL (1994). Aggregate stability and rain impacted sheet erosion of air in dried and pre-wetted clayey surface soils under intense rain. Soil Sci. 158: 321-330

 

Molope MN, Page ER, Grieve TC, (1985). A comparison of soil aggregate stability using soil with different cultivation histories, Comm. Soil Sci. Plant Anal. 16: 315-322

 

Neves CSVJ, Feller C, Guimaraes MF, Medina CC Tavares Filho J, Fortier M (2003) Soil bulk density and porosity of homogeneous morphological units identified by the cropping profile  method in clayey Oxisols in Brazil. Soil Till. Res. 71: 109-119.

 

Nimmo JR, Perkins KS, (2002). Aggregate stability and size distribution, In: Dane JE,Topp GC (eds) Mehtod of soil analysis part 4 physical methods, Soil, 53.

 

Nweke IA (2015c). Effect of land use on organic matter concentration of aggregate fractions of fallow and cultivated soils. Indian Journal of Applied Research, Volume 5(3): 507-512.

 

Nweke IA, Nnabude PC, (2014). Aggregate size distribution and stability of aggregate fractions of fallow and cultivated soils, J. Experimental Biol. Agric. Sci. 1 (7 special issue): 515-520

 

Nweke IA, Nnabude PC, (2015a). Aggregate stability of four soils as evaluated by different indices, J. Experimental Biol. Agric. Sci. 3(3): 246-252.

 

Nweke IA, Nnabude PC, (2015b). Colloidal stability and potential structural deformation index of four Nigerian soils, Amer. J. Experimental Agric. 5(3): 239-251.

 

Panayiotopoulos KP, Kostopoulou T (1989). Aggregate stability dependence on size cultivation and various soil constituents in red Mediterranean soils (Alfisols), Soil Tech. 2:59- 69.

 

Piccolo A, Mbagwu JSC, (1994). Humic substances and surfactants effects on the stability of two tropical soils, Soil Sci. Soc. Amer. 58: 950-955

 

Walkley A, Black IA, (1934). An examination of the Degtjarf method for determining soil organic matter and a proposed modification of the chronic acid titration method, Soil Sci. 37: 29-38.

 

Yoder RE, (1936). A direct method of aggregate analysis and a study of the physical nature of erosion losses J. Amer. Soc. Agron. 28: 337-351.