Until the introduction of fertilizers in the 19th century nutrient-poo
r conditions prevailed in the larger part of The Netherlands. Freshwat
er wetlands consequently were of nutrient-poor nature. During the firs
t half of the 20th century many surface waters gradually eutrophied, b
ut most waters in the Pleistocene area and even some polders in the Ho
locene area kept their nutrient-poor conditions. Only during the last
decades virtually all waters became eutrophied or polluted. The main s
ources of nutrients are agriculture, precipitation and water from the
large rivers.