Abstract:This study was carried out to evaluate the physicochemical properties of topsoil from forest development area. The results of physicochemical properties of topsoil from forest development area shown on the average loamy sand~sandy clay loam in soil texture, 5.3~7.1 in pH, 0.02~0.18 dS/m in EC, 0.7~1.8% in OM, 0.03~0.11% in T-N, 11~15 cmol
“…국내 산지초지에 관한 연구는 토양의 이화학적 특성과 목초의 생산성에 대한 연구 들이 주로 진행되어 왔다 (Hur and Leung, 1997;Jung, 1992;Jung and Rim, 2001;Kim et al, 2012;Lee, 1997) (Hwang and Jang, 1994;Zhang et al, 2006;Zhang et al, 2010 (Choi, 1986;Um et al, 1992;Zhang, 1998) (Table 3).…”
This study deals with the distribution of the clay minerals separated from clay fractions of ranch pastures in Korea and their chemical and mineralogical properties. Crystalline phases of the clay minerals were identified by powder X-ray diffraction (XRD) pattern and FT-IR spectra, and their relative chemical compositions were also analyzed by X-ray flourescence spectrometry (XRF). Primary minerals consisted mainly of quartz and mica and chlorite and kaolinite along with a trace of swelling micas were identified as secondary clay minerals. However, the relative content of these clay minerals was different with the locations, which led to significant effects on physical and chemical properties of soils like inorganic elemental composition. In particular, SiO 2 content was higher in Gochang ranch pasture than in other ranch pasture. Infrared (IR) spectra did not indicate any significant differences in organic functional groups among the locations. This study clearly showed that ranch pastures had different relative content of clay minerals and chemical properties depending on the location and consequently that those properties are worthy to be taken into account for soil amendment.
“…국내 산지초지에 관한 연구는 토양의 이화학적 특성과 목초의 생산성에 대한 연구들이 주로 진행되어 왔다 (Hur and Leung, 1997;Jung, 1992;Jung and Rim, 2001;Kim et al, 2012;Lee, 1997) (Hwang and Jang, 1994;Zhang et al, 2006;Zhang et al, 2010 (Choi, 1986;Um et al, 1992;Zhang, 1998) (Table 3).…”
This study deals with the distribution of the clay minerals separated from clay fractions of ranch pastures in Korea and their chemical and mineralogical properties. Crystalline phases of the clay minerals were identified by powder X-ray diffraction (XRD) pattern and FT-IR spectra, and their relative chemical compositions were also analyzed by X-ray flourescence spectrometry (XRF). Primary minerals consisted mainly of quartz and mica and chlorite and kaolinite along with a trace of swelling micas were identified as secondary clay minerals. However, the relative content of these clay minerals was different with the locations, which led to significant effects on physical and chemical properties of soils like inorganic elemental composition. In particular, SiO 2 content was higher in Gochang ranch pasture than in other ranch pasture. Infrared (IR) spectra did not indicate any significant differences in organic functional groups among the locations. This study clearly showed that ranch pastures had different relative content of clay minerals and chemical properties depending on the location and consequently that those properties are worthy to be taken into account for soil amendment.
“…In addition, increasing soil organic matter levels can reduce atmospheric CO2 levels that contribute to climate change. Therefore, healthy soil gives us clean air and water, bountiful crops and forests, productive grazing lands, diverse wildlife, and beautiful landscapes (Park et al, 2008 (Cho and Kim, 2000;Kim et al, 2012).…”
This study was carried out to evaluate the physicochemical properties and perform a feasibility analysis of planting material composed of topsoil from river improvement and non-improvement areas. The results showed that the physicochemical properties of topsoil from river improvement areas were on the average sandy loam~loamy sand in soil texture, 5.6~6. , and 3~171 mg/kg in Av. P2O5. Meanwhile, the results of an applied valuation of topsoil-based planting were as follows. Ex. K + levels were low grade in all survey areas. OM was low grade in 12 improvement areas and 11 non-improvement areas.Av. P2O5 levels were low grade in 10 improvement areas and 10 non-improvement areas. T-N was low grade in six improvement areas and four non-improvement areas. Ex. Mg 2+ levels were low grade in two improvement areas.
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