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Relevant bibliographies by topics / Soils – Zimbabwe

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Journal articles

Academic literature on the topic 'Soils – Zimbabwe'

Author: Grafiati

Published: 4 June 2021

Last updated: 6 February 2022

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Journal articles on the topic "Soils – Zimbabwe"

1

Nyamapfene, K. W. "Some relationships between topography and sodic soils in Zimbabwe." Zeitschrift für Geomorphologie 30, no. 1 (1986): 47–52. http://dx.doi.org/10.1127/zfg/30/1986/47.

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2

Jones, U. S., and M. Piha. "Evaluation of four soil test extractants for Zimbabwe soils." Communications in Soil Science and Plant Analysis 20, no. 17-18 (1989): 1857–71. http://dx.doi.org/10.1080/00103628909368188.

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3

MAPFUMO, P., S. MPEPEREKI, and P. MAFONGOYA. "PIGEONPEA RHIZOBIA PREVALENCE AND CROP RESPONSE TO INOCULATION IN ZIMBABWEAN SMALLHOLDER-MANAGED SOILS." Experimental Agriculture 36, no. 4 (2000): 423–34. http://dx.doi.org/10.1017/s0014479700001009.

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A study was conducted to determine the population sizes of indigenous pigeonpea (Cajanus cajan)-nodulating rhizobia and responses of the crop to rhizobial inoculation in soils under smallholder management. Rhizobia populations were determined in 21 soils from three different agro-ecological regions of Zimbabwe using the plant infection most-probable-number technique. Pigeonpea response to rhizobial inoculation was tested in five soils representative of low, medium and high rhizobia populations. Pigeonpea rhizobia ranged from undetectable to 121 cells per g soil compared with 16 to 159 cells pe

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4

Mapaure, I. "A floristic classification of the vegetation of a forest-savanna boundary in southeastern Zimbabwe." Bothalia 27, no. 2 (1997): 185–93. http://dx.doi.org/10.4102/abc.v27i2.680.

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The vegetation of Chirinda Forest boundary was classified into eight types using Two-way Indicator Species Analysis (TWINSPAN) and Detrended Correspondence Analysis (DCA). The moist forest comprises three types: Strychnos mellodora-Chrysophyllum gonmgosanum Forest on deep dolerite soils; Chrysophyllum gorungosanum-Myrianthus holstii Forest on shallow dolerite soils; and Teclea iiobilis-Ehretia cymosa Forest on drier, but deep dolerite soils. The non-forest vegetation comprises five types: Themeda triandra Grassland on shallow dolerite soils; Psidium guajava Bushland on sandstone; Bridelia micr

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5

Twomlow, S. J. "Field moisture characteristics of two fersiallitic soils in Zimbabwe." Soil Use and Management 10, no. 4 (1994): 168–73. http://dx.doi.org/10.1111/j.1475-2743.1994.tb00481.x.

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6

MUJURU, L., L. RUSINAMHODZI, J. NYAMANGARA, and M. R. HOOSBEEK. "Effects of nitrogen fertilizer and manure application on storage of carbon and nitrogen under continuous maize cropping in Arenosols and Luvisols of Zimbabwe." Journal of Agricultural Science 154, no. 2 (2015): 242–57. http://dx.doi.org/10.1017/s0021859615000520.

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SUMMARYSoil organic matter (SOM) is important for long-term crop productivity through maintenance of soil quality and is also now receiving attention due to its potential for climate change mitigation. The objectives of the present study were to investigate the effects of 9 years of fertilization on soil organic carbon (SOC) and total organic nitrogen (TON) and their fractions for the 0–50 cm profile in clayey (Luvisols) and sandy (Arenosols) soils in Murewa District, Zimbabwe. Three treatments were assessed: unfertilized (Control), nitrogen fertilizer (Nfert) and nitrogen fertilizer plus catt

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7

Mugabe, F. T., M. G. Hodnett, and A. Senzanje. "Effect of temporal rainfall distribution and soil type on soil moisture and runoff generation in semi-arid Zimbabwe." Hydrology Research 38, no. 3 (2007): 249–63. http://dx.doi.org/10.2166/nh.2007.014.

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This paper examines the effect of temporal rainfall distribution on soil moisture and runoff generation in the 5.9 km2 Mutangi catchment in semi-arid Zimbabwe. Rainfall, soil moisture and runoff were measured during the 1999/00 and 2000/01 rainy seasons during which periods 755 mm and 615 mm of rainfall were received, respectively. The percentage of rainfall totals in these periods were 58% and 69%, respectively, in February. The total catchment runoff was 102 mm and 63 mm, of which 52% and 49% were recorded over 6 and 4 d in 2000 and 2001, respectively. Baseflow was negligible. Rainfall inten

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8

Cooper, G. R. C. "Oxidation and toxicity of chromium in ultramafic soils in Zimbabwe." Applied Geochemistry 17, no. 8 (2002): 981–86. http://dx.doi.org/10.1016/s0883-2927(02)00014-8.

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9

Scoones, Ian. "Landscapes, fields and soils: understanding the history of soil fertility management in Southern Zimbabwe." Journal of Southern African Studies 23, no. 4 (1997): 615–34. http://dx.doi.org/10.1080/03057079708708560.

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10

Mukungurutse, Collis, Newton Nyapwere, Amos Manyanga, and Luke Mhaka. "Pedological Characterization and Classification of Typical Soils of Lupane District, Zimbabwe." International Journal of Plant & Soil Science 22, no. 3 (2018): 1–12. http://dx.doi.org/10.9734/ijpss/2018/39609.

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