https://doi.org/10.36873/aev.v1

A. Journal
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引用次数: 1

Abstract

ABSTRACTRed-yellow podzolic soil is widespread in West Kotawaringin and mostly used as agricultural land. It causechanges in soil properties so that soil fertility analysis is needed. The research aims to study the chemistry andphysics of red-yellow podzolic, as a result of agricultural activities. The research was conducted by taking soilsamples from unmanaged land (control land) and oil palm plantations belong to KUD Tani Subur which appliedoil palm integration with cows in Pangkalan Lada, Central Kalimantan. In this study we conducted simple randomsampling method with 5 replications. Variables used as parameter in the study are porosity, bulk density, pH, Ctotal, N-total, P-available, Cation Exchange Capasity (CEC), base saturation (BS), Fe, and Al-exchangeable. Theresults show oil palm plantations have soil porosity 51,84%, bulk density 1,28 g cm-3, pH soil about 5,02-5,04;C-total 1,23-1,69%; N- total%; 0,06-0,11%, P-available 8,1-8,9 ppm; CEC 18,52-22,85 me 100g-1; BS 1,79-3,24; Fe 0,59-0,82 ppm; and Al- exchangeable 110,46-111,29 ppm, but control land have soil porosity 45,03%;bulk density 1,46 g cm-3; pH 5,04-5,13; C-total 0,76-1,05; N-total 0,09-0,19; P- available 9,3-9,7 ppm; CEC20,30-22,27 me 100g-1; BS 2,33-2,76%; Fe 0,02-0,68 ppm; and Al-ec 126,67-156,60 ppm. Land use of RYP soiltypes as oil palm plantations with semi- organic processing techniques does not degrade the soil, and couldincrease land productivity compared to unmanaged land.Keywords: RYP, soil chemistry and physics, different land use.
https://doi.org/10.36873/aev.v1
摘要/ abstract摘要:黄灰化土在西达科他州分布广泛,主要用作农业用地。它会引起土壤性质的变化,因此需要对土壤肥力进行分析。该研究旨在研究农业活动导致的红黄灰化病的化学和物理特性。研究人员从加里曼丹中部邦卡兰拉达(Pangkalan Lada)的未管理土地(对照土地)和KUD Tani Subur的油棕种植园采集土壤样本,该种植园将油棕与奶牛进行整合。本研究采用5个重复的简单随机抽样方法。研究中使用的参数变量包括孔隙度、容重、pH、Ctotal、n total、p available、阳离子交换容量(CEC)、碱饱和度(BS)、Fe和al交换性。结果表明:油棕人工林土壤孔隙度为51.84%,容重为1.28 g cm-3, pH值为5.02 - 5.04,总碳量为1.23 -1,69%;N -总%;0,06-0,11%, P-available 8,1-8,9 ppm;CEC 18、52-22、85 me 100g-1;BS 79 - 3, 24;Fe 0,59-0,82 ppm;和铝交换态分别为110、46 ~ 111、29 ppm,而对照地土壤孔隙度为45.03%,容重为1.46 g cm-3;pH值5 04-5 13;C-total 0, 76 - 1, 05年;n总0 09-0 19;P-可选9,3-9,7 ppm;CEC20、30-22、27me 100g-1;BS 2 33-2 76%;Fe 0,02-0,68 ppm;Al-ec 126,67-156,60 ppm。采用半有机加工技术的RYP土壤类型作为油棕种植园的土地利用不会使土壤退化,与未管理的土地相比,可以提高土地生产力。关键词:RYP,土壤理化,不同土地利用方式。
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