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Estimating the submarine groundwater and nutrients discharge of Yellow River delta with cross-section method.

机译:用断面法估算黄河三角洲海底地下水和养分流量。

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In this paper, cross-section method was used to estimate the groundwater and nutrients discharge fluxing to the Bohai Sea from the Yellow River Delta. The flux of shallow phreatic groundwater (within 10 m) in the Yellow River Farm discharging into sea was 2.9x10(-5) m3/m d in 2004 and 3.1x10(-5) m3/m d in 2005. Time distribution monthly mean flux is consistent with the Yellow River's runoff but taking on lag effect. And the volume of the phreatic water discharging from the whole delta is 3.71-3.77x10(3) m3, which is 2x10(-5)% of the Yellow River's annual runoff. The transport amount of shallow confined water (buried depth 15-20 m) from 2004 to 2005 was 5.7-6.2x10(-3) m3/m d in the Yellow River delta, 0.0037-0.004% of the runoff of Yellow River. There is low concentration of NO3-, NH4+ and PO4(3-) but high dissolved SiO2 in the shallow confined aquifer. Despite the high concentration of phreatic nitrate, it weakly influences the seawater because of the little flux of discharge into sea.
机译:本文采用截面法估算了黄河三角洲向渤海排放的地下水和养分流量。黄河农场入海浅水潜水(10 m以内)的通量在2004年为2.9x10(-5)m3 / md,在2005年为3.1x10(-5)m3 / md。时间分布月平均通量为与黄河的径流一致,但有滞后效应。整个三角洲的潜水水排放量为3.71-3.77x10(3)m3,占黄河年径流量的2x10(-5)%。 2004年至2005年,浅水承压水(埋深15-20 m)的输送量在黄河三角洲为5.7-6.2x10(-3)m3 / m d,占黄河径流量的0.0037-0.004%。浅层承压含水层中NO3-,NH4 +和PO4(3-)的浓度较低,但SiO2的溶解度较高。尽管潜水硝酸盐浓度很高,但由于排放到海洋的通量很少,因此对海水的影响很小。

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