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The enrichment of 137 Cs in the soil loss from small agricultural watersheds
Author(s) -
Weigand Stephan,
Schimmack Wolfgang,
Auerswald Karl
Publication year - 1998
Publication title -
zeitschrift für pflanzenernährung und bodenkunde
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.644
H-Index - 87
eISSN - 1522-2624
pISSN - 0044-3263
DOI - 10.1002/jpln.1998.3581610414
Subject(s) - sediment , surface runoff , erosion , environmental science , soil water , phosphorus , environmental chemistry , deposition (geology) , nutrient , total organic carbon , hydrology (agriculture) , chemistry , soil science , geology , ecology , paleontology , geotechnical engineering , organic chemistry , biology
Enrichment ratios (ER) are widely used to predict loss of sorbed nutrients or pesticides with runoff sediment, while ER is frequently neglected in studies which quantify past erosion from global fallout 137 Cs losses. The ER of 137 Cs (ER‐ 137 Cs) in the soil loss and the subsequent depletion of 137 Cs at the soil surface were determined for eight small watersheds (1.6–16.8 ha) with different soils and land use. Due to preferential loss of the clay fraction, the upper 5 mm of the soil surface was significantly depleted of 137 Cs after a heavy storm. A total of 31 watershed‐events were investigated with soil losses ranging between 1.2 and 480 kg‐ha −1 and sediment concentrations between 1.98 and 54.1 gṁL −1 The correspondent ER‐ 137 Cs (mean: 1.72, range: 0.40–4.95) was positively correlated to the ER of clay, organic carbon, total nitrogen and calcium‐acetate‐lactate‐extractable phosphorus (P CAL ). A close correlation between ER‐ 137 Cs and ER‐P CAL was also found for sediment samples of detention ponds, where most of the ER values were less than 1.0 due to depletion. Therefore, ER‐P CAL seems to be a suitable estimate of ER‐ 137 Cs for both, erosion and deposition processes. Our findings strongly support the need for considering ER‐ 137 Cs, when ,37 Cs data are used to assess rates and pattern of soil redistribution. Otherwise, soil loss will be overestimated in a range of about factor 2 in many cases.