【摘要】 为了进一步探索重富营养化湖泊水质形成机理，１９９６年７月１９日－９月２日，在太湖北端湖湾重富营养化水体──五里湖中层水体进行了试验。通过对微分方程的积分与数理统计分析，确定了该湖区该时段平均沉降通量为４０５ｇｄ^－１ｍ^－２，其中有机质沉降通量是无机沉降通量的 ３倍，有机质初始分解率为０．０１２　５１ｈ^－１，长期分解率为 ０．００６ ６２ｈ^－１，１个月的时间就有８０％的有机质分解掉。这种作用造成许多重富营养化湖泊，当悬浮物以死亡的藻类为主时，就会出现透明度低而叶绿素并不高的现象；藻类死亡后，逐步沉降并矿化分解，其残体与矿化物又可返回水体，其中的营养盐又被新生的藻类再次吸收利用，导致富营养化湖泊水质的变化长期处于恶性循环，这一现象在当前富营养化湖泊的治理中应予重视。更多还原

【Abstract】 In order to explore furthter the water-quality-change mechnism in hypertrophic lakes, the test was undertaken for the griddle water layer in hypertrophic Wulihu Bay, northern Taihu Lake, during the period from July 19 to September 2 in 1996. On the basis of differential-equation integration calculus and mathmatical and physical statistics, it was found that in this part of the lake during the pened the downward flux was 405 gd^-1 m^-2 on average, and that the downward organic fluxes were three times more than the downward inorganic fluxes. The initial decomposition rate of organic substances is about 0.012 51 h^-1, and the long-term decomposition rate is 0.006 62 h^-1, the instantaneous decomposition rate (D, h^-1) may be described by the following eqution: D = 0.006 624 1+0.005 859e^{-0.006 624 1t}, where t is bine （h）. Around 80% of the organic substance was decomposited within a mouth. In many hypertrophic lakes it appears that transparency is low and chlorophyll-a is not high when suspended substances are domained by dead algae. After algae die, they drop progressively, mineralize and are decomposed simultaneously, then the remains and mineralized substances retum to water body, and the nutrientS are absorbed and utilized by the newborn algae. Thus, the water quality changes are for long periods in vicious circles in the hypertrophic lake. The effects of rinsing and dredging ect, which cannot break the vicious circle, are not very ideal. The phenomenon should be taken into account during harnessing the present hypertrophic lake.更多还原