| soil_data | R Documentation |
A hypothetical dataset representing soil physicochemical and biological properties across five land-use systems and two soil depths, generated using realistic parameter ranges reported in the soil quality literature. This dataset is intended for demonstrating the functions in the SQIpro package and for pedagogical purposes.
soil_data
A data frame with 100 rows and 14 variables:
Character. Land-use system: Natural_Forest,
Agroforestry, Cropland, Grassland,
Degraded_Land.
Character. Soil depth: Surface_0_15cm or
Subsurface_15_30cm.
Numeric. Soil pH (1:2.5 water suspension). Unitless. Optimal range 6.0–7.0 for most crops (Brady & Weil, 2008).
Numeric. Electrical Conductivity (dS m^{-1}).
Lower values indicate less salinity stress; <0.2 dS m^{-1}
considered non-saline (Richards, 1954).
Numeric. Bulk Density (g cm^{-3}). Lower values
indicate better soil structure and aeration; >1.6 g cm^{-3}
restricts root growth (Arshad et al., 1996).
Numeric. Cation Exchange Capacity
(cmol(+) kg^{-1}). Higher values indicate greater
nutrient-holding capacity (Sparks, 2003).
Numeric. Organic Carbon (%). Higher values indicate greater soil organic matter, a key indicator of soil health (Doran & Parkin, 1994).
Numeric. Microbial Biomass Carbon
(mg kg^{-1}). Indicator of soil biological activity
(Brookes, 1995).
Numeric. Potentially Mineralizable Nitrogen
(mg kg^{-1}). Indicates N-supplying capacity of soil
(Stanford & Smith, 1972).
Numeric. Clay content (%). Optimal range 20–35% for water and nutrient retention (Arshad et al., 1996).
Numeric. Water Holding Capacity (%). Higher values indicate better moisture retention (Reynolds et al., 2009).
Numeric. Dehydrogenase Enzyme Activity
(\mug TPF g^{-1} day^{-1}). Indicator of
overall microbial metabolic activity (Casida et al., 1964).
Numeric. Available Phosphorus (mg kg^{-1}).
Higher values indicate better P availability for plants
(Olsen & Sommers, 1982).
Numeric. Total Nitrogen (%). Higher values indicate greater N reserves (Bremner, 1996).
Parameter ranges were informed by values reported in:
Doran and Parkin (1994) for biological indicators
Andrews et al. (2004) for MDS indicator ranges
Masto et al. (2008) for land-use comparison ranges
The dataset is entirely synthetic and does not represent any specific geographic location.
Synthetically generated for the SQIpro package.
Andrews, S.S., Karlen, D.L., & Cambardella, C.A. (2004). The soil management assessment framework: A quantitative soil quality evaluation method. Soil Science Society of America Journal, 68(6), 1945–1962. \Sexpr[results=rd]{tools:::Rd_expr_doi("10.2136/sssaj2004.1945")}
Arshad, M.A., Lowery, B., & Grossman, B. (1996). Physical tests for monitoring soil quality. In J.W. Doran & A.J. Jones (Eds.), Methods for Assessing Soil Quality, pp. 123–141. SSSA Special Publication 49. \Sexpr[results=rd]{tools:::Rd_expr_doi("10.2136/sssaspecpub49.c7")}
Brady, N.C., & Weil, R.R. (2008). The Nature and Properties of Soils (14th ed.). Prentice Hall, New Jersey.
Doran, J.W., & Parkin, T.B. (1994). Defining and assessing soil quality. In J.W. Doran et al. (Eds.), Defining Soil Quality for a Sustainable Environment, pp. 1–21. SSSA Special Publication 35. \Sexpr[results=rd]{tools:::Rd_expr_doi("10.2136/sssaspecpub35.c1")}
Masto, R.E., Chhonkar, P.K., Singh, D., & Patra, A.K. (2008). Alternative soil quality indices for evaluating the effect of intensive cropping, fertilisation and manuring for 31 years in the semi-arid soils of India. Environmental Monitoring and Assessment, 136, 419–435. \Sexpr[results=rd]{tools:::Rd_expr_doi("10.1007/s10661-007-9697-z")}
data(soil_data)
head(soil_data)
summary(soil_data)
table(soil_data$LandUse, soil_data$Depth)
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