Svojstva poljoprivrednih tala su pod dominantnim utjecajem agrotehničkih zahvata. Provedbom tih zahvata, neka se svojstva tla dugoročno pogoršavaju. Prenamjenom prirodnog tla u poljoprivredno, često dolazi i do pojačane erozije. Erozijom može doći do promjena u strukturi i teksturi tla, zbog kojih se mogu mijenjati i brojna druga svojstva tla. Stoga je cilj ovog rada bio istražiti u kojoj mjeri način korištenja zemljišta i nagib terena od 12% utječu na značajke pseudogleja obronačnog na obiteljskom gospodarstvu Šipek u Donjoj Zelini. Dodatni cilj bio je ispitati da li su svojstva pseudogleja na oranici izmijenjena u tolikoj mjeri, da se to tlo može svrstati u oranično semiterestrično tlo (sensu Husnjak, 2014). Sondiranjem su istražena četiri profila tla, od čega dva na gornjem, a dva na donjem dijelu padine (udaljenost između gornjeg i donjeg dijela padine bila je 50 m). Pritom je, na svakom dijelu padine, jedan profil istražen na prije tridesetak godina napuštenom poljoprivrednom zemljištu (livada), a drugi na oranici. Utvrđena su temeljna svojstva tla (morfologija tla, mehanički sastav tla, reakcija tla i parametri adsorpcijskog kompleksa tla, sadržaj humusa, sadržaj fiziološki aktivnog fosfora i kalija). Utvrđeno je da se, unatoč različitim načinima korištenja zemljišta, istražena tla međusobno razlikuju samo u ograničenoj mjeri (ponajprije u različitom sadržaju hraniva). Zaključeno je da, nakon što se tlo prestane koristiti za biljnu proizvodnju, njegova svojstva vrlo sporo dolaze u ravnotežu s prirodnim faktorima pedogeneze, tj. uvjetima okoliša. Stoga se i tlo na oranici i tlo na livadi mogu svrstati u oranično semiterestrično tlo. Zbog odnošenja materijala tijekom pedogeneze, nagib terena je uvjetovao povećanje ekološke dubine tla duž istražene padine. Naime, na gornjem dijelu obronka, na dubini tla 80-110 cm, utvrđen je stariji, znatno glinovitiji i zbijeniji horizont, u odnosu na horizonte iznad njega. Recentni tokovi materijala niz padinu općenito su neznatno utjecali na istražena svojstva tla. Stoga se može zaključiti da, u uvjetima humidne klime, na padinama dužine do oko 50 m i nagiba do oko 12%, erozija na praškasto ilovastim tlima nema uvijek značajan utjecaj na svojstva tla. Ipak, potrebno je provesti istraživanje s većim brojem opažanja (kako duž padine, tako i unutar pojedinih segmenata padine), i to na padinama različitih dužina. Također, utjecaj erozije tla treba procjenjivati pri raznovrsnim načinima korištenja zemljišta, odnosno pri različitim sustavima obrade tla., Properties of agricultural soils are dominantly affected by agro-technical interventions. These interventions lead to deterioration of some soil properties in the long run. Conversion of natural soil into agricultural soil also often leads to enhanced erosion. Erosion may induce changes in soil structure and texture, thus affecting a number of other soil properties. Hence, the aim of this study was to asses the extent to which both land use and 12% slope inclination affect properties of Pseudogley on slope at the Šipek family farm in Donja Zelina. Additional aim was to investigate whether, on ploughland, the properties of the studied Pseudogley changed to the extent that this soil could be systemized as Ploughland semi-terrestrial soil (sesu Husnjak, 2014). Four soil profiles were investigated by auger. Two of these profiles were on the upper part of the slope, and two were on the lower part of the slope (the distance between the two parts of the slope was 50 m). On both parts of the slope, one profile was on an agricultural land abandoned some 30 years ago (meadow), and the other was on a ploughland. Basic soil properties were determined (soil morphology, particle size distribution, pH and parameters of the adsorption complex, humus content, physiologically active phosphorus and potassium) contents. It was noted that the different land uses caused the soils to differ one from the other only to a limited extent (most notably, in soil nutrients contents). It was inferred that, once soil stopped being used as a ploughland, it regained balance with natural soilforming factors (i.e., with environmental conditions) very slowly. Hence, both the soil on the polughland and the soil on the meadow may be systemized as Ploughland semi-terrestrial soils. Inclination caused the increase of the ecological soil depth along the slope. Namely, due to washout during pedogenesis, on the upper part of the slope, at the depth of 80-110 cm, we observed an older, more clayey and more compacted horizon, compared with the above-lying horizons. Recent flows of material down the slope affected soil properties only slightly. It appears that, in humid climate, on slopes that are up to about 50 m long and up to about 12% inclined, erosion on silt loam soils does not always significantly impact soil properties. However, this should be confirmed by using a higher number of observations (both along the slope and within the slope segments) on slopes with differing lengths. Further, soil erosion should be assessed across various land uses, i.e., across different soil tillage systems.