Soil chemical and physical properties as indicators of sustainable land management under sugar cane in Papua New Guinea

Abstract

The sustainability of land management was assessed for a sugar cane plantation using soil Ž . chemical and physical properties as indicators. The plantation 6000 ha was established in 1979 on a broad alluvial plain and the majority of the soils are classified as Eutric and Mollic Fluvisols Ž . Ž . 73% and Eutric Vertisols 23% . Average annual rainfall is about 2000 mm with a dry season Ž from May to November. The sugar cane is not irrigated and receives only N fertilizer 90 kg N y1 y1 . Ž . ha yr . Detailed soil maps were used to make a selection 186 samples of the existing soil Ž . chemical database [1979][1980][1981][1982][1983][1984][1985][1986][1987][1988][1989][1990][1991][1992][1993][1994] and for selecting sample sites in 1996. The pH of the topsoils had decreased from about 6.5 to 5.8 in both Fluvisols and Vertisols accompanied by a decrease in CEC and exchangeable K. Between 1979 and 1996, organic C contents declined from about 5.5 to y1 Ž y1 . 3.2 g kg . A significant decline in available P was found in Fluvisols 40 to 32 mg kg and Ž y1 . Vertisols 37 to 25 mg kg . Significant changes in soil chemical properties were mostly confined to the topsoil and differences between Fluvisols and Vertisols were relatively small. Changes in soil physical properties were assessed by measuring bulk density and infiltration under sugar cane and adjoining natural grassland areas. Bulk density and water intake were similar under natural grassland and within the sugar cane rows. The interrow had a significantly higher bulk density due to wheel traffic, which caused very low water intake. Bulk densities at which infiltration rates were severely reduced were slightly higher in Fluvisols than in Vertisols but for both Major Soil Groupings an increase of only 0.2 Mg m y3 was critical. Changes in soil chemical and physical properties indicated that land management is not sustaining the resource base for sugar cane cultivation in the long-term. Threshold values in soil chemical properties were not reached and they were in 1996 still favourable for sugar cane cultivation. The soil compaction, however, directly affect the sugar cane as it seriously reduce rooting. It is concluded that routine ) Fax: q675-4757380; E-mail: ahartemink@ag.unitech.ac.pg 0016-7061r98r$19.00 q 1998 Elsevier Science B.V. All rights reserved.Ž . PII S0016-7061 98 00048-2 ( ) A.E. Harteminkr Geoderma 85 1998 283-306 284 soil analytical data combined with data that can be easily collected suffices to make a general assessment of sustainable land management at a plantation scale. q 1998 Elsevier Science B.V. All rights reserved.

Propriedades físicas de um Latossolo Vermelho distrófico cultivado e sob mata nativa

“…A maior Ds nos solos cultivados está relacionada com a compactação do solo pelo tráfego de máquinas e implementos (Hajabbasi et al,1997;Hartemink, 1998;Cavenage et al, 1999), com a redução dos teores de matéria orgânica (Silva & Kay, 1997;Dalal & Chan, 2001) e com a menor estabilidade da estrutura do solo (Horn et al, 1995). O aumento da densidade do solo na área cultivada também pode ser explicado pela redução nos teores de matéria orgânica em comparação com o solo sob mata nativa.…”

Effect of land use on soil nutrients in the loess hilly area of the Loess Plateau, China

“…These include soil physical, chemical and/or biological properties (Nambiar et al, 2001;Arshad and Martin, 2002;Doran, 2002;Mulugeta et al, 2005). Their changes may be assessed by measuring and comparing present values against the values at the commencement of the monitoring period (Arshad and Martin, 2002), historical data when available (Hartemink, 1998), and soil properties under reference ecosystems (Feigl et al, 1995;Wang and Gong, 1998), or by using values measured at different time intervals (Mulugeta et al, 2005).…”

Efeito da qualidade da água de irrigação sobre os atributos físicos de um neossolo flúvico do Município de Quixeré, CE - Brasil

“…Assim, os valores de Ds entre 1,37 e 1,55 Mg m -3 (Quadro 6) são característicos de solos sob efeito de sais, concordando com os dados de Macêdo & Santos (1992), quando registraram Ds variando entre 1,45 e 1,47 Mg m -3 em solos aluviais irrigados com água salina, e com as observações de Saunders et al (1982), que observaram para a mesma classe de solos Ds média de 1,57 Mg m -3 . Hartemink (1998) (a)…”