Comparison of soil and sediment properties of a loamy sand soil

Fullen, Michael A.; Zheng, Ya; Brandsma, R.T.

doi:10.1016/0933-3630(95)00041-0

Cited by 31 publications

(27 citation statements)

References 20 publications

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“…Though not the subject of presented paper, Ca and Mg losses by water erosion are usually high (e.g. Fullen et al 1997;Bertol et al 2003;Zhang et al 2004b) and their removal can affect soil pH. Treatment erosion rates were variable and base cation loss could have an influence on differences in original soil pH between treatments.…”

Section: Resultsmentioning

confidence: 95%

“…Since the recorded soil erosion is always higher under low density crops, the effects on the environment may be more pronounced (Lal 2006;Pimentel 2006 Gachene et al 1997) show increase of nutrients in soil sediments in addition to non-eroded soil, while others find the opposite. For example, Fullen et al (1997) and Zhang et al (2004a) find lower organic matter, phosphorus and nitrogen content and lower pH values in sediment than in the non-eroded soil. Recently, the majority of soil erosion research has been focused on sampling the sediments and runoff after rainfall simulations (e.g.…”

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confidence: 97%

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Effects of soil erosion by water under different tillage treatments on distribution of soil chemical parameters

Kisić¹,

Bogunović²,

Zgorelec³

et al. 2018

Soil Water Res.

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Section: Resultsmentioning

confidence: 95%

mentioning

confidence: 97%

Effects of soil erosion by water under different tillage treatments on distribution of soil chemical parameters

Kisić¹,

Bogunović²,

Zgorelec³

et al. 2018

Soil Water Res.

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“…This was also observed by and Kisic et al (2002) for enrichment of clay and OC, respectively. On the other hand, Fullen (1991) and Fullen et al (1996) found lower OC, clay, and silt concentrations in eroded material compared with the loamy sand topsoil and attributed it to eluviation of clay and organic matter into the topsoil during runoff events. This in-washing process resulted in a "fi ltration pavement" immediately beneath the surface crust.…”

mentioning

confidence: 97%

Enrichment of Organic Carbon in Sediment Transport by Interrill and Rill Erosion Processes

Schiettecatte

Gabriëls

Cornelis

et al. 2008

Soil Science Soc of Amer J

153

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Erosion and loss of organic carbon (OC) result in degradation of the soil surface. Rill and interrill erosion processes on a silt loam soil were examined in laboratory rainfall and flume experiments. These experiments showed that rill and interrill erosion processes have contrasting impacts on enrichment of OC in transported sediment. Rill erosion was found to be nonselective, while for interrill erosion the enrichment ratio of OC, EROC, varied between 0.9 and 2.6 and was inversely related to the unit sediment discharge. At unit sediment discharge values >0.0017 kg s−1 m−1, the EROC remained equal to 1. The enrichment process was not influenced by raindrop impact. Enrichment of OC by “aggregate stripping” was found to be unimportant in our study. This was attributed to the low aggregate stability of the soil and the equal distribution of OC within the different soil aggregate classes.

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“…Organic matter was removed for laser-diffraction particle size study. Pretreatments for grain-size analysis frequently use oxidative treatments (Buurman, Pape, & Muggler, 1996;Fullen, Zheng, & Brandsma, 1996;Scott-Jackson & Walkington, 2005;Wang, Jin, Bu, Zhou, & Wu, 2006). All of the samples were mixed with a dispersing agent (.3% sodium hexametaphosphate) in order to disperse the clay particles.…”

Section: Loss-on-ignition and Grain-size Analysesmentioning

confidence: 99%

Reconstructing mid-to-recent Holocene paleoenvironments in the vicinity of ancient Amarynthos (Euboea, Greece)

et al. 2012

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This article examines the shoreline evolution and human occupation in the vicinity of the important archeological site of Amarynthos (Euboea Island, Greece) over the last six millennia. Archeological evidence indicates a continuous occupation of the site from the Bronze Age to the Roman period and the site is well-known, thanks to the existence of a sanctuary dedicated to the goddess Artemis. Based on the study of four boreholes, a paleogeographic reconstruction of the coastal landscape is proposed. Facies were determined based on mollusc identification, and sedimentology based on grain-size measurements (hand sieving for the fraction above 2 mm and LASER technique for particles below 2 mm) and loss-on-ignition. In addition, a series of 12 AMS radiocarbon dates define a reliable chronostratigraphy. Results suggest the presence of a fully marine environment from the early Holocene to ca. 2600-2400 cal. BC, which developed into a brackish environment from ca. 2600-2400 cal. BC to ca. 750 cal. BC due to the deltaic progradation of the nearby stream (Sarandapotamos River). From ca. 750 cal. BC onward, coastal swamps prevailed in the study area. Human-environmental interaction is discussed and particular attention is paid to the paleolandscape configuration of Amarynthos.

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Comparison of soil and sediment properties of a loamy sand soil

Cited by 31 publications

References 20 publications

Effects of soil erosion by water under different tillage treatments on distribution of soil chemical parameters

Effects of soil erosion by water under different tillage treatments on distribution of soil chemical parameters

Enrichment of Organic Carbon in Sediment Transport by Interrill and Rill Erosion Processes

Reconstructing mid-to-recent Holocene paleoenvironments in the vicinity of ancient Amarynthos (Euboea, Greece)

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