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首页> 外文期刊>Journal of Applied Aquaculture >Physical and chemical characteristics of soil from tiger shrimp aquaculture ponds at Malacca, Malaysia
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Physical and chemical characteristics of soil from tiger shrimp aquaculture ponds at Malacca, Malaysia

机译:马六甲马六甲虎虾水产养殖池塘土壤的理化特征

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Soil physicochemical properties of the growout ponds of black tiger shrimp {Penaeus monodon) were examined in relation to shrimp yields for one production cycle. The culture ponds were old (>5 years) and new (newly constructed) types. Soil texture wassilty clay with low sand content and high proportion of clay for both the pond types with alkaline soil pH (7.87-9.71). Organic matter (OM) concentration was higher (7.48 ± 0.01%) in old ponds and positively related (r = 0.58, P < 0.05) with total nitrogen (TN). The major cations (Ca, Mg, and Na) were higher in the soil of old ponds and did not fluctuate significantly during culture. The majority of trace elements, i.e., Fe (349.22 ± 35.7 ppm), Mn (56.19 ± 30.2 ppm), Zn (88.56 ± 8.09 ppm), Al (454.3 ± 200.6), Pb (1.3 ± 0.96 ppm), Co (3.4 ± 0.2), V (6.56 ± 1.79 ppm), Cr (19.32 ± 0.63 ppm), Ti (82.78 ± 54.3 ppm), As (5.60 ± 0.28 ppm), Ag (0.38 ± 0.5 ppm), and Sb (3.89 ± 0.48 ppm) were found to be higher in new pond soils than the old ponds.Except for soil manganese, no major fluctuations in trace elements were observed during the culture period. Shrimp growth was not significantly different in the two types of ponds, and no distinct correlation between shrimp growth and element content ofsoils could be drawn. The results indicate that shrimp pond age may not affect production of shrimp if soils are properly managed pre- and postcul-ture. The differences in production in different ponds might be the result of management practice such asquality of shrimp post larvae, pond preparation, water and feed quality, and available live feed in the pond bottom or other environmental factors like water nutrients and physicochemical parameters.
机译:对一个生产循环的虾产量,研究了黑虎虾(Penaeus Monodon)的生长池塘的土壤理化性质。文化池塘旧(> 5年),新建(新建)类型。土壤纹理Wassilty粘土与低砂含量和高比例粘土,含碱土壤pH(7.87-9.71)。有机物(OM)浓度高(7.48±0.01%)在旧池塘中较高,呈正相关(R = 0.58,P <0.05),具有全氮(TN)。在旧池塘的土壤中,主要阳离子(Ca,Mg和Na)较高,文化期间没有显着波动。大多数微量元素,即Fe(349.22±35.7 ppm),Mn(56.19±30.2 ppm),Zn(88.56±8.09​​ ppm),Al(454.3±200.6),Pb(1.3±0.96ppm),CO(3.4 ±0.2),V(6.56±1.79ppm),Cr(19.32±0.63 ppm),Ti(82.78±54.3 ppm),AS(5.60±0.28ppm),Ag(0.38±0.5ppm)和Sb(3.89±0.48在新的池塘土壤中发现ppm比旧池塘的土壤较高。在锰锰的except中,在文化期间没有观察到微量元素的重大波动。两种类型的池塘中虾生长没有显着差异,并且可以拉出虾生长和元素含量之间的明显相关性。结果表明,如果土壤被适当地管理预期和后期治疗,虾池池肠肠龄可能不会影响虾的产生。不同池塘生产的差异可能是管理实践的结果,如虾柱,池塘准备,水和饲料质量,以及池塘底部或其他环境因素的可用活饲料,如水营养素和物理化学参数。

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