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laboratory incubation studies, compared the release of<br />

nukrients frm (A) pl--it zakeri-1 cut in October and (B) fc*<br />

ous produced by sheep fed the same mterials cut at monthly<br />

intervals Prom May to October. He found that readily<br />

available nitrogen (N), inchding urine N, increased from<br />

31.5 for A t o 52.7 kg ha-' for B for krcstia-Fesf uoa<br />

a d 12.0 for. A to 18.4 for 3 kg nal for Nardus in spite<br />

of herbage producLion decreases of 6% for A and 24% for B.<br />

Similar reault s were found for phosphorus (P)-<br />

He also<br />

demonstrated increased uptake of N and P fim dung and urine<br />

by the pasture plants,<br />

Clearly, gr~zing speeds up the<br />

nutrient circulation in the surfaca soil./vegetatiun system<br />

and this more rapid re-use of the small amounts of available<br />

nutrients present in hill soils can be interpreted aa an<br />

jndication of improved soil fertility,<br />

In his fence-line study, Floate (1972) found that grazing led<br />

to:<br />

i) Reductions in the ratios of c.rrSon (c) to N and P for phnt<br />

rewins and of soil to 4O cm depth. Such ratio& are<br />

often thought of as indicatcrr s of soil fert;iUty.<br />

a) Increases, in b &la total and organic P but no significant<br />

ohange in the concent ration of available P in the top 40 cm<br />

iii) mPn herease in soil pK but not in base saturation,<br />

Howard & Howard (1 976) recorded higher nitrogen cronteflts and<br />

a lower C/N ratio in the top 3.5 cm of eoil Kith grueingn<br />

bspi rntory actidty of the soils was higher on the ungmz#d<br />

area, probably as a result of conversion of herbage to faeces<br />

with a lower mspiratory activity (Floate, 1970). During<br />

& Radoliffe (1962) found th~t the top 4 cn of the duneenriched<br />

soil of sheep-tmcks on hills In New Zealand had is. higher C

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