Abstract
Application of organic amendments to soil is commonplace in domestic gardening. However, a vast array of materials could be labelled as ‘compost’ by retailers and suppliers. We investigated six different amendments currently used, or available for use, in horticulture: composted bark, composted bracken, spent mushroom compost, composted horse manure, garden waste compost (at two different application rates), and peat. Using a controlled field experiment, we examined the physicochemical differences between the amendments, the subsequent effects on soil characteristics, and resultant yield and biometrics of Lavatera trimiestris. Amended soils resulted in a significantly different multivariate soil environment and N budget when compared to the unamended control. However, the effect on yield and plant biometrics (number of flowers, plant height, etc.) depended on the amendment used. Application of garden compost resulted in up to a five-fold increase in yield. However, there was no significant difference in yields in soils amended with composted bark or peat, when compared to the unamended control. This has implications, as there is increasing pressure to remove peat from products available to domestic gardeners. The variability in the different amendments investigated in our research, in addition to the variable effects on plant growth parameters, suggests that repeated use of a single amendment may not be best practise for gardeners.
Highlights
The site consisted of 3 m × 3 m plots in a randomised complete block alignment (8 blocks, 8 replicates) treated annually with the following amendments: Irish moss peat (Peat); composted horse manure (HM), garden compost at full rate (GCf) and half rate (GCh) from collected prunings and cuttings from Royal Horticultural Society (RHS) Wisley
Content, etc.), and subsequent analysis of similarity (ANOSIM) show that each amendment is significantly different from one another (Table 2)
Physicochemical Properties of Organic Amendments Commonly Used in Horticulture
Summary
Both commercial and domestic horticulturalists recognise that soil organic matter (SOM) is critical for plant production [1]. The presence of SOM can stimulate the growth of plants sown in the medium both directly, through stimulating seed germination and root initiation [2,3], and indirectly through improving soil characteristics favourable for subsequent plant growth. Such as provision of nutrients, improved soil structure and water holding capacity [3,4,5]. In agriculture and commercial horticulture, a number of practices can enhance
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