Loess soils are among the most fertile in the world, principally because th
e abundance of silt particles ensures a good supply of plant-available wate
r, good soil aeration, extensive penetration by plant roots, and easy culti
vation and seedbed production. Also micaceous minerals in the silt and clay
fractions provide an adequate supply of potassium for most crops. and the
large amounts of total nitrogen in chernozems can maintain moderate yields
of cereals without fertilizer additions, However, loess soils often contain
little clay, which leads to loss of organic matter from soil types other t
han chernozems under arable cultivation; the resulting structural instabili
ty of the surface soil causes problems of crusting, poor germination of cro
ps and erosion. This paper reviews early opinions of the fertility of loess
, and summarises later scientific assessments of loess soils in USA, China,
eastern Europe and Britain. In regions of thin but fairly extensive loess
deposits, such as UK and parts of USA, loess probably plays an important ro
le in maintaining yields of arable crops, and needs special measures to pro
tect it from the increasing erosion noted in recent decades. (C) 2001 Elsev
ier Science B.V. All rights reserved.